"Exp"	"Site"	"Hole"	"Core"	"Type"	"Section"	"A/W"	"Sample ID"	"Offset top (cm)"	"Offset bottom (cm)"	"Top depth CSF-A (m)"	"Middle depth CSF-A (m)"	"Bottom depth CSF-A (m)"	"Top depth CSF-B (m)"	"Middle depth CSF-B (m)"	"Bottom depth CSF-B (m)"	"Domain no."	"Piece no."	"Lithologic unit"	"Summary of igneous features"	"Summary of alteration features"	"Summary of structural features"	
"399"	"U1601"	"C"	"2"	"R"	"1"	""	"399-U1601C-2R-1"	"0.0"	"80.0"	"23.000"	"23.400"	"23.800"	"23"	"23.4"	"23.8"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with relatively low opx abundance and trace cpx, with two diabase pebbles on top."	"Highly altered slightly vesicular basalt at the top of the section (0-9.5 cm). Phenocrysts are completely replaced by secondary minerals, possibly chlorite. The fine-grained nature of the rock makes it difficult the recognition of igneous minerals. Strongly serpentinized harzburgite dominates downhole."	"Serpentinized protogranular harzburgite with two generations of orthopyroxene, cut by a weak subhorizontal serpentine foliation. Thin diabase recovered between 0-10 cm. The section shows weak- to moderate- veining, dominated by inclined to subvertical dipping little white veins.  F (serp) > M > V1"	
"399"	"U1601"	"C"	"2"	"R"	"2"	""	"399-U1601C-2R-2"	"0.0"	"84.0"	"23.800"	"24.220"	"24.640"	"23.8"	"24.22"	"24.64"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with relatively low opx abundance and trace spinel and cpx."	"Highly serpentinized harzburgite. Mesh and chrysotile veins are present. Chrysotile locally grades to massive picrolite suggesting concomitant crystallization."	"Serpentinized protogranular harzburgite with two generations of orthopyroxene, cut by a weak subhorizontal serpentine foliation.   The section shows weak- to moderate- veining, dominated by steep to subvertical (68-77 cm) little white veins.  F (serp) > M >  V1"	
"399"	"U1601"	"C"	"3"	"R"	"1"	""	"399-U1601C-3R-1"	"0.0"	"115.0"	"27.900"	"28.475"	"29.050"	"27.9"	"28.475"	"29.05"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Alternating intervals of harzburgite, opx-bearing dunites, and dunites at ~10cm scale, all with spinel."	"Highly to completely serpentinized harzburgite and Opx-bearing dunite. Mesh and chrysotile veins are present."	"Serpentinized protogranular to porphyroclastic harzburgite and dunite; harzburgite shows subhorizontal weakly foliated, patchy regular to no mesh; dunite has moderstely dipping (43°), foliated mesh. Section cut by a set of moderate to steeply dipping white veins. "	
"399"	"U1601"	"C"	"3"	"R"	"2"	""	"399-U1601C-3R-2"	"0.0"	"97.0"	"29.050"	"29.535"	"30.020"	"29.05"	"29.535"	"30.02"	""	"1, 2, 3, 4"	""	"Dunite with a middle harzburgite 35 cm thick. Has a basal opx-bearing dunite layer bounded by olivine websterites. Spinel was found in all units."	"Highly to completely serpentinized harzburgite and Opx-bearing dunite cut by two intervals of Ol-websterite. A dark corona is developed around interstitial orthopyroxene. Adjacent mesh texture after olivine appears brown stained. In Ol-websterite, serpentine forms after olivine and orthopyroxene and amphibole after clinopyroxene, respectively. Opx-bearing dunite and Ol-websterite are cut by serpentine-magnetite and late chrysotile."	"Dunite and serpentinized harzburgite.  Dunite hosts subhorizontal (10°) weakly foliated to no mesh.  Protogranular serpntinized harzburgite with regular patchy mesh.  Section cut by several vein types including magmatic, white and black with moderate to steep dips, and  60° plunging slickenfibers, overall cut by subvertical and subhorizontal thin white (crysotile) veins. F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"4"	"R"	"1"	""	"399-U1601C-4R-1"	"0.0"	"134.0"	"32.700"	"33.370"	"34.040"	"32.7"	"33.37"	"34.04"	""	"1, 2"	""	"Opx-bearing dunite continued from the last section at the top, underlain by a dunitic interval with a Cr-spinel trail at the center (23cm). From 33-66 cm is a harzburgite interval followed by an opx-bearing dunite with trace cpx and spinel."	"Highly to completely serpentinized Opx-bearing dunite and minor harzburgite. Spinel appears less altered than silicates in chromite-rich layers. In Opx poor areas, Opx is completely altered; where Opx is more abundant, it is less altered. Bastite after Opx is greenish brown. Bastite after interstitial Opx is grey-colored. Two vein types can be distinguished: serpentine-magnetite in mesh texture and chrysotile veins."	"Protogranular to weak protoclastic serpentinized harzburgite with dunite (10- 32cm) and orthopyroxene-bearing dunite (70-89 cm) intervals. Chromite layer in dunite with a SPO parallel to the boundary (dip 45°). Elongate orthopyroxene define a weak mantle fabric dipping 45-55°. No foliation of the serpentine mesh. Section cut by serpentine-magnetite and younger steeply dipping (75°) serpentine veins. F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"4"	"R"	"2"	""	"399-U1601C-4R-2"	"0.0"	"132.0"	"34.040"	"34.700"	"35.360"	"34.04"	"34.7"	"35.36"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Opx-bearing dunite continuous from previous section, underlain by harzburgite then opx-bearing dunite, all with trace cpx and spinel."	"Highly serpentinized Opx-bearing dunite and harzburgite. Towards the bottom of the section mesh texture after olivine shows a brown stain. Serpentine-magnetite veins in mesh texture and chrysotile-picrolite veins are present."	"Protogranular serpentinized harzburgite with a subhorizontal orthopyroxene-bearing dunite (38-57 cm) interval. Patchy subhorizontal serpentine mesh folation cut by moderate dip (40-50°) green black and white veins. F (mantle) > F (serp) > V1"	
"399"	"U1601"	"C"	"5"	"R"	"1"	""	"399-U1601C-5R-1"	"0.0"	"127.0"	"37.600"	"38.235"	"38.870"	"37.6"	"38.235"	"38.87"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Harzburgite unit with trace cpx and spinel."	"Completely serpentinized and highly weathered dunite and strongly serpentinized harzburgite. Vein types include serpentine-magnetite veins in mesh texture cut by chrysotile veins, as well as late carbonate and carbonate-serpentine veins."	"Serpentinized protogranular harzburgite between 53-77, 86-27 cm; other intervals show no fabric due to alteration. Intensity of serpentine mesh folation increases down section from 0 at 0-76 cm, to strong at 127cm. The section shows weak- to moderate- veining, dominated by subhorizontal crysotile and mt-crysotile veins cuts by subvertical zeolite veins.  Green serpentine piece side vein w/  slickenfibers plunging 15° (52-76 cm).  F (serp) > V1 >V2"	
"399"	"U1601"	"C"	"6"	"R"	"1"	""	"399-U1601C-6R-1"	"0.0"	"107.0"	"42.400"	"42.935"	"43.470"	"42.4"	"42.935"	"43.47"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with varying proportions of granular and interstitial opx and trace spinel and cpx. "	"Highly serpentinized and partially weathered Cpx-bearing harzburgite. Weathering after serpentinization is indicated by brown and reddish patches locally associated with carbonate (aragonite) veins. Opx is less altered than olivine in weathered patches. Serpentine-magnetite veins in mesh texture, chrysotile veins, and late carbonate veins occur in this section. Carbonate veins also contain clasts of the serpentinite host."	"Serpentinized protogranular harzburgite with patchy to regular serpentine mesh texture developed.  The section shows weak- to moderate- density veining, dominated by subhorizontal to inclined crysotile veins cuts by subvertical zeolite veins. F (serp) > V1 >V2"	
"399"	"U1601"	"C"	"6"	"R"	"2"	""	"399-U1601C-6R-2"	"0.0"	"69.0"	"43.470"	"43.815"	"44.160"	"43.47"	"43.815"	"44.16"	""	"1, 2, 3"	""	"Harzburgite with varying proportions of granular and interstitial opx and trace spinel ands cpx, continuous from previous section. 2 cm dunite interval at 54cm."	"Highly serpentinized Cpx-bearing harzburgite. Mesh and chrysotile veins are the main vein types observed in this section."	"Protogranular to weakly foliated (subhorizontal) porphyroclastic  serpentinized harzburgite with regular patchy to weakly foliated serpentine mesh texture (0-10° dip). Section cut by moderate to steeply dipping, thin crysotile veins. F (mantle) > V1"	
"399"	"U1601"	"C"	"7"	"R"	"1"	""	"399-U1601C-7R-1"	"0.0"	"136.0"	"47.300"	"47.980"	"48.660"	"47.3"	"47.98"	"48.66"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Opx-bearing dunite with varying proportions of opx. Has a  dunite interval between 62 and 86 cm with patches of Cr-spinel."	"Highly to completely serpentinized Cpx-bearing harzburgite and Opx-bearing dunite. Harzburgite is variably weathered. Areas around former Opx show yellow staining. Mesh texture shows reddish brown staining. Serpentine-magnetite veins related to mesh formation and late chrysotile(-picrolite) veins occur in this section. Some of the thicker serpentine-magnetite veins are partially oxidized forming Fe-hydroxides."	"Protogranular to porphyroclastic serpentinized harzburgite and dunite, with subhorizontal, regular patchy to weakly foliated mesh. Cut by a series of shallow to steeply dipping white veins. "	
"399"	"U1601"	"C"	"8"	"R"	"1"	""	"399-U1601C-8R-1"	"0.0"	"70.0"	"52.100"	"52.450"	"52.800"	"52.1"	"52.45"	"52.8"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Opx-bearing dunite continuous from previous section, underlain by harzburgite with a crosscutting highly altered gabbroic domain."	"Highly to completely serpentinized harzburgite crosscut by light-colored veins of possible magmatic origin. The latter are hydrothermally overprinted. Close to these veins, mesh texture after olivine appears black. Hydrothermal assemblages after magmatic veins might be composed of carbonate (dolomite or magnesite). They also contain an unidentified light brown, fibrous, mineral (hardness above 5) and a white mineral (hardness between 5 and 6). Other types of veins include serpentine-magnetite, chrysotile, and carbonate veins."	"Serpentinize protogranular to weakly porphyroclasitic (50° dip) serpentinized harzburgite, with weak to strongly developed patchy regular mesh. Section cut by a moderate dip, branched magmatic vein, in turn cut by steeply dipping crysotile veins (5-21 cm), subhorizontal crysotile veins (29-36 cm), steeply dipping (69°) green/white fibrous veins and subhorizontal picrolite veins (40-59 cm). F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"9"	"R"	"1"	""	"399-U1601C-9R-1"	"0.0"	"102.0"	"57.000"	"57.510"	"58.020"	"57"	"57.51"	"58.02"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Opx-bearing dunite with mostly interstitial opx, underlain by a harzburgite unit with mostly intestitial opx, and then another harzburgite unit with mostly granular opx. Trace spinel is found throughout. Cpx is present beneath 33.5 cm."	"Highly serpentinized harzburgite. Serpentne-magnetite veins in mesh texture. Later chrysotile veins are cut by composite carbonate-serpentine veins. The latter generally occurs on piece edges."	"Protogranular to weak protoclastic serpentinized harzburgite with a weak, subhorizontal mantle fabric, and variable, but locally well-developed subhorizontal patchy regular to moderate- and strongly foliated (subhorizontal) serpentine mesh. Section cut by subhorizontal to vertical white-green veins and one late carbonate vein (4-7 cm).  F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"9"	"R"	"2"	""	"399-U1601C-9R-2"	"0.0"	"132.0"	"58.020"	"58.680"	"59.340"	"58.02"	"58.68"	"59.34"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with both granular and interstitial opx and trace cpx and spinel. "	"Highly serpentinized harzburgite. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins."	"Protogranular serpentinized harzburgite with patchy regular mesh, cut by steep (80° dip)white-green veins in turn cut by horizontal white veins. F (serp) > V1"	
"399"	"U1601"	"C"	"9"	"R"	"3"	""	"399-U1601C-9R-3"	"0.0"	"143.0"	"59.340"	"60.055"	"60.770"	"59.34"	"60.055"	"60.77"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with both granular and interstitial opx and trace cpx and spinel. "	"Highly serpentinized harzburgite. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins."	"Protogranular serpentinized harzburgite, with patchy regular mesh, cut by steep to moderate dip veins."	
"399"	"U1601"	"C"	"10"	"R"	"1"	""	"399-U1601C-10R-1"	"0.0"	"88.0"	"61.800"	"62.240"	"62.680"	"61.8"	"62.24"	"62.68"	""	"1, 2, 3"	""	"Harzburgite with both granular and interstitial opx, and trace amount of spinel and cpx."	"Highly serpentinized harzburgite. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins."	"Protogranular serpentinized harzburgite, lacking any fabric.  Section cut by gently dipping white veins, and shallow to moderate dip white and green veins.  "	
"399"	"U1601"	"C"	"10"	"R"	"2"	""	"399-U1601C-10R-2"	"0.0"	"94.5"	"62.680"	"63.153"	"63.625"	"62.68"	"63.153"	"63.625"	""	"1, 2, 3"	""	"Harzburgite and opx-bearing dunite with olivine websterite veins. "	"Alternating intervals of highly serpentinized Cpx-bearing harzburgite, Opx-bearing dunite, and Ol-websterite. In the later, mesh after Ol appears black. Several vein types including mesh and chrysotile veins"	"Protogranular to weakly porphyroclastic (horizontal mantle fabric) serpentinized harzburgite, with coarse grained websterite (3 cm thick) and dunite intervals with moderate dipping contacts.  Dunite host with a moderate- to strongly foliated mesh (moderate dip). Dunite bands cut by moderate dip crysotile veins (55° dip).  "	
"399"	"U1601"	"C"	"10"	"R"	"3"	""	"399-U1601C-10R-3"	"0.0"	"146.0"	"63.625"	"64.355"	"65.085"	"63.625"	"64.355"	"65.085"	""	"1, 2, 3, 4"	""	"Dunite with up to 1% spinel and with olivine websterite veins. Dunite grades into harzburgite with trace cpx and spinel at c. 28 cm."	"Highly serpentinized Cpx-bearing harzburgite and Opx-bearing dunite crosscut by serpentinized Ol-websterite. In the later, mesh after Ol appears black. Several vein types including mesh and chrysotile veins."	"Dunite, websterite, and serpentinized harzburgite with ~30° contacts.  Serpentinized harzburgite is protogranular to weakly porphyroclastic subhorizontal mantle fabric.  Dunite has moderately foliated mesh with gentle to moderate dips.  White and green veins with shallow to moderate dips. F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"10"	"R"	"4"	""	"399-U1601C-10R-4"	"0.0"	"132.5"	"65.085"	"65.748"	"66.410"	"65.085"	"65.748"	"66.41"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with mostly granular opx. Trace spinel and cpx."	"Highly serpentinized Cpx-bearing harzburgite crosscut by several veins of possible magmatic origin that are hydrothermally overprinted. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins and chlorite-carbonate veins."	"Weakly protoclastic serpentinized harzburgite with regular patchy mesh, cut by two magmatic veins with moderate to steep dips.  White and green veins with moderate dips.  Subhorizontal little white veins.  F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"11"	"R"	"1"	""	"399-U1601C-11R-1"	"0.0"	"121.0"	"66.700"	"67.305"	"67.910"	"66.7"	"67.305"	"67.91"	""	"1, 2, 3, 4"	""	"Harzburgite with mostly granular opx and trace spinel and 3% cpx."	"Highly serpentinized Cpx-bearing harzburgite. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins."	"Weakly porphyroclastic serpentinized harzburgite with regular mesh. Upper part of the section (0-42 cm) cut by subhorizontal thin white crysotile veins. F (mantle) > V1 "	
"399"	"U1601"	"C"	"11"	"R"	"2"	""	"399-U1601C-11R-2"	"0.0"	"93.0"	"67.910"	"68.375"	"68.840"	"67.91"	"68.375"	"68.84"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Opx-bearing dunite with granular opx and trace spinel. Piece #3 (12-21) has a highly altered, disseminated oxide gabbronorite domain."	"Highly serpentinized Opx-bearing dunite crosscut by a altered magmatic vein. Mesh texture in serpentinized peridotite close to the vein appears black. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins. Carbonate veins, locally associated with sulfides, represent the last vein generation."	"Protogranular  to weakly porphyroclastic serpentinized harzburgite, with subhorizontal mantle fabric and patchy regular mesh. Section but by steep magmatic vein, steep green vein, and gently dipping green vein, cut by a moderately dipping white vein.  "	
"399"	"U1601"	"C"	"12"	"R"	"1"	""	"399-U1601C-12R-1"	"0.0"	"121.0"	"71.500"	"72.105"	"72.710"	"71.5"	"72.105"	"72.71"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25"	""	"Opx-bearing dunite section containing highly altered gabbro and oxide gabbro domains."	"Completely serpentinized Opx-bearing dunite cut by altered magmatic veins. The mesh texture close to the magmatic veins is black. Secondary hydrothermal (white, light-brown, and grey) minerals in the altered magmatic vein could not be identified. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile-picrolite veins."	"Protogranular serpentinized harzburgite with patchy regular mesh. Dunite interval between 101- 121 cm with weakly foliated mesh developed. Section cut by two rhodingitized magmatic veins at 15-21 and 100-107 cm, cut subhorizontal to gently dipping green-white veins. M > V1"	
"399"	"U1601"	"C"	"12"	"R"	"2"	""	"399-U1601C-12R-2"	"0.0"	"56.0"	"72.710"	"72.990"	"73.270"	"72.71"	"72.99"	"73.27"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Opx-bearing dunite with trace spinel and containing a disseminated oxide gabbronorite domain at c. 17 cm.  "	"Highly serpentinized Opx-bearing dunite cut by altered (grey to white) magmatic veins composed of prehnite and other unidentified minerals. Close to the veins, the mesh texture appears black. Mesh texutre appears grey-white further away from the veins.  Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins."	"Protogranular serpentinized harzburgite, no to regular, patchy mesh."	
"399"	"U1601"	"C"	"13"	"R"	"1"	""	"399-U1601C-13R-1"	"0.0"	"110.0"	"76.400"	"76.950"	"77.500"	"76.4"	"76.95"	"77.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21"	""	"Opx-bearing dunite unit with up to 1 % spinel and containing a disseminated oxide gabbronorite domain at 43.5-61cm, and an orthopyroxenite domain at 91-110cm."	"Highly serpentinized Opx-bearing dunite cut by veins of possible magmatic origin. Mesh texture after olivine next to the magmatic vein appears black.  Serpentine-magnetite veins in mesh texture are crosscut by chrysotile, chlorite-serpentine, and late carbonate veins."	"Protogranular serpentinized harzburgite, with patchy regular mesh."	
"399"	"U1601"	"C"	"13"	"R"	"2"	""	"399-U1601C-13R-2"	"0.0"	"70.0"	"77.500"	"77.850"	"78.200"	"77.5"	"77.85"	"78.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Opx-bearing dunite with both granular and interstitial opx, and trace amounts of cpx and spinel. "	"Highly serpentinized Opx-bearing dunite crosscut by one vein of possible magmatic origin. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile and picrolite veins."	"Serpentinized harzburgite with protogranular to strongly foliated, horizontal, porphyroclastic fabric, with weak to patchy regular mesh.  Moderately dipping magmatic vein.  White and green veins with gentle to moderate dips. F (mantle) > F (serp) > V1 > V2 "	
"399"	"U1601"	"C"	"14"	"R"	"1"	""	"399-U1601C-14R-1"	"0.0"	"96.0"	"81.200"	"81.680"	"82.160"	"81.2"	"81.68"	"82.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Opx-bearing dunite with both granular and interstitial opx and trace amoiunts of cpx and spinel."	"Highly serpentinized Opx-bearing dunite crosscut by a vein of possible magmatic origin. The mesh texture is black close to the magmatic vein at the bottom of the section. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile and picrolite veins."	"Strongly porphyroclastic erpentinized harzburgite with subhorizontal mantle fabric, and no to patchy regular mesh.  Cut by moderately dipping magmatic vein, vertical white vein and horizontal little white veins. F (mantle) > F (serp) > V1 > V2"	
"399"	"U1601"	"C"	"14"	"R"	"2"	""	"399-U1601C-14R-2"	"0.0"	"89.0"	"82.160"	"82.605"	"83.050"	"82.16"	"82.605"	"83.05"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with trace spinel underlain by altered, medium-grained gabbronorite."	"Highly serpentinized harzburgite and almost fresh gabbronorite at the bottom of the section. At the contact with the gabbronorite, the mesh texture appears black. The serpentinized harzburgite is crosscut by chrysotile and picrolite veins."	"Protogranular serpentinized harzburgite ith moderate dip (50°) weakly foliated mesh. Gabbro interval, mostly isotropic with one protomylonitic rubble piece.  Two veins, one moderately dipping, the other steep. F (mantle) > V1 > V2"	
"399"	"U1601"	"C"	"15"	"R"	"1"	""	"399-U1601C-15R-1"	"0.0"	"134.0"	"86.100"	"86.770"	"87.440"	"86.1"	"86.77"	"87.44"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25"	""	"Opx-bearing dunite with granular and minor interstitial opx, underlain at c. 67 cm by relatively fresh harzburgite. Both peridotites have trace cpx and spinel. A 2mm-wide gabbro vein cuts the dunite"	"Highly serpentinized harzburgite (top of the section) and Opx-bearing dunite (bottom of the section) crosscut by pale pink to beige veins of probable magmatic origin. Moderately altered basalt is present at 4-7 cm. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile, chlorite, picrolite, and late composite carbonate-serpentine-pyrite veins."	"Thin interval (4-7 cm) of diabase in protogranular to strongly porphyroclastic (horizontal mantle fabric) serpentinized harzburgite, with patchy regular mesh.  Section cut by moderate dip magmatic veins, shallow to moderate black-white-green veins.  Sub-horizontal little white veins. F (mantle) > F (serp) > V1 > V2 > V3"	
"399"	"U1601"	"C"	"16"	"R"	"1"	""	"399-U1601C-16R-1"	"0.0"	"143.0"	"90.900"	"91.615"	"92.330"	"90.9"	"91.615"	"92.33"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26"	""	"Opx-bearing dunite with trace spinel underlain by harzburgite with trace spinel and cpx. Gabbro veins up to 3 mm in width form a domain throughout this section."	"Variably serpentinized Opx-bearing dunite and harzburgite, locally displaying areas with fresh olivine in the mesh cores. The peridotites are crosscut by magmatic veins that are hydrothermally overprinted. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile and picrolite veins. "	"Protogranular serpentinized harzburgite with patchy regual to weakly foliated mesh (25° dip). Section cut by several magmatic vein with  moderate to steep dips, cut by green and white veins with shallow to moderate dips. F (serp) > V1 > V2 > V3"	
"399"	"U1601"	"C"	"16"	"R"	"2"	""	"399-U1601C-16R-2"	"0.0"	"143.0"	"92.330"	"93.045"	"93.760"	"92.33"	"93.045"	"93.76"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with interstitial opx underlain by opx-bearing gabbro that contains a dunitic interval. Gabbro veins up to 3 mm in width form a domain between 110-135 cm in this section."	"Variably serpentinized Opx-bearing dunite and harzburgite, locally displaying areas with fresh olivine in the mesh cores. The peridotites are crosscut by magmatic veins that are hydrothermally overprinted. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile, picrolite, chrysotile-picrolite, and late carbonate-serpentine veins."	"Protogranular serpentinized harzburgite with patchy regular mesh. Orthopyroxene-bearing dunite interval (127-144 cm) with a gently dipping contact. Section cut several magmatic veins with moderate to steep dips,   green veins with moderate dip, and subhorizontal little white vein..  F (serp) > V1 > V2 > V3"	
"399"	"U1601"	"C"	"16"	"R"	"3"	""	"399-U1601C-16R-3"	"0.0"	"150.0"	"93.770"	"94.520"	"95.270"	"93.77"	"94.52"	"95.27"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Section of opx-bearing dunite with trace spinel and cpx. The dunite is cut by microgabbro (51-74) and disseminated oxide gabbro (108-131)."	"Highly serpentinized Opx-bearing dunite crosscut by two intervals consisting of moderately to completely altered gabbro. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile, picrolite, and chrysotile-picrolite veins. The latter locally cut the gabbro."	"Protogranular to weakly porphyroclastic (horizontal mantle fabric) serpentinized harzburgite with patchy regular to subhorizontal, weakly foliated mesh.  Gabbro interval is isotropic to mylonitic with 20° dip.  Cut by white and green veins with moderate dip. M  > V1 > V2"	
"399"	"U1601"	"C"	"17"	"R"	"1"	""	"399-U1601C-17R-1"	"0.0"	"150.0"	"95.800"	"96.550"	"97.300"	"95.8"	"96.55"	"97.3"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28"	""	"Opx-bearing dunite with a small proportion of spinel. Olivine is relatively fresh."	"Almost completely serpentinized Opx-bearing dunite crosscut by altered magmatic veins. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins. "	"Protogranular serpentinized harzburgite with subhorizontal regular to weakly foliated mesh. One moderately dipping magmatic vein, one steeply dipping white vein."	
"399"	"U1601"	"C"	"17"	"R"	"2"	""	"399-U1601C-17R-2"	"0.0"	"140.0"	"97.300"	"98.000"	"98.700"	"97.3"	"98"	"98.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"Opx-bearing dunite with relatively fresh olivine and trace spinel. Gabbronorite veins crosscut at 88-92cm and 117-130cm."	"Almost completely serpentinized Opx-bearing dunite crosscut by altered magmatic veins. Towards the veins, the mesh texture appears black. Serpentine-magnetite veins in mesh texture are cut by chrysotile, picrolite, and late carbonate veins. Some of these veins locally the magmatic veins."	"Protogranular to weakly prophyroclastic (horizontal) serpentinized harzburgite with pathcy regualr to weakly foliated mesh (5° dip).  Cut by several magmatic veins, moderate dips, cut by white green veins, moderate dip."	
"399"	"U1601"	"C"	"18"	"R"	"1"	""	"399-U1601C-18R-1"	"0.0"	"149.0"	"100.600"	"101.345"	"102.090"	"100.6"	"101.345"	"102.09"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Opx-bearing dunite continuous from the previous section with a highly-altered gabbro domain."	"Almost completely serpentinized Opx-bearing dunite crosscut by hydrothermally overprinted magmatic veins. Close to the veins, the mesh texture appears black. Several vein generations include chrysotile, picrolite locally containing oxide, and late carbonate veins that locally reopen former serpentine veins. These veins postdate hydrothermally overprinted magmatic veins and mesh formation."	"Protogranular serpentinized harzburgite with no to regualr patchy to weakly foliated mesh (10° dip).  Steep magmatic fabric.  Moderately dipping white, gray, green vein."	
"399"	"U1601"	"C"	"18"	"R"	"2"	""	"399-U1601C-18R-2"	"0.0"	"123.0"	"102.090"	"102.705"	"103.320"	"102.09"	"102.705"	"103.32"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Harzburgite with trace spinel, and with gabbronorite and oxide gabbro domains. "	"Almost completely serpentinized Opx-bearing dunite crosscut by hydrothermally overprinted magmatic veins. Close to the veins, the mesh texture appears black. Several vein generations include chrysotile, picrolite locally containing oxide, and late carbonate veins that locally reopen former serpentine veins. These veins postdate hydrothermally overprinted magmatic veins and mesh formation."	"Protogranular serpentinized harzburgite with weakly foliated to unfoliated serpentine mesh. Grey veins intruded by anastomosing network of green veins. white vein at 75-79cm and grey vein at 92-96cm are sheared with locally weak crystal plastic foliation. little white veins throughout are sometimes cross cut by little green veins."	
"399"	"U1601"	"C"	"18"	"R"	"3"	""	"399-U1601C-18R-3"	"0.0"	"84.0"	"103.320"	"103.740"	"104.160"	"103.32"	"103.74"	"104.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with mostly interstitial opx underlain by opx-bearing dunite with varying abundances of opx. "	"Almost completely serpentinized Opx-bearing dunite and minor harzburgite crosscut by magmatic veins that have been hydrothermally overprinted. Close to the vein, the mesh texture after olivine appears black. Serpentine-magnetite veins in mesh texture are crosscut by chrysotile veins. "	"Protogranular serpentinized harzburgite, no mesh to 19cm, non-foliated mesh 19cm to bottom of the section. Grey veins with 35° dip cut/followed by dark green veins and white veins."	
"399"	"U1601"	"C"	"19"	"R"	"1"	""	"399-U1601C-19R-1"	"0.0"	"150.0"	"105.500"	"106.250"	"107.000"	"105.5"	"106.25"	"107"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"This section is orthopyroxene-bearing dunite and harzburgite with trace chromium spinel. Thin veins of highly altered gabbro or gabbronorite traverse the peridotites centered at 2, 41, 65, 120, and 128 cm. "	"Partially to completely serpentinized harzburgite interspersed with hydrothermally altered mafic veins. "	"Protogranular to weakly porphyroclastic serpentinized harzburgite. Locally developed mesh. Contact with dunite with steep to moderate dip. Cut by magmatic, green, grey-white, and white veins with shallow to moderate dips, and one vertical dip. A magmatic vein is sheared, and have shallow dip.  "	
"399"	"U1601"	"C"	"19"	"R"	"2"	""	"399-U1601C-19R-2"	"0.0"	"139.0"	"107.000"	"107.695"	"108.390"	"107"	"107.695"	"108.39"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"This section is mostly orthopyroxene-bearing dunite, with harzburgite from 0-7 cm. Highly altered gabbronorite crosses the section from 25.5 to 30 cm."	"Partially to completely serpentinized harzburgite and minor dunite interspersed with hydrothermally altered mafic veins."	"Porphyroclastic serpentinized harzburgite (20° dipping mantel fabric), with foliated mesh. Cut by white-green steep vein and horizontal to inclined white vein."	
"399"	"U1601"	"C"	"19"	"R"	"3"	""	"399-U1601C-19R-3"	"0.0"	"128.0"	"108.390"	"109.030"	"109.670"	"108.39"	"109.03"	"109.67"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is mainly orthopyroxene-bearing dunite with mostly interstitial grains. Orthopyroxene modal abundance decreases down section. The dunite is cut by orthopyroxenite veins particularly in pieces 1 and 4."	"Partially to completely serpentinized Opx-bearing dunite interspersed with hydrothermally altered mafic veins."	"Serpentinized harzburgite with local weak porphyroclastic fabric and moderate serp mesh (20° dipping mantle fabric). Subvertical magmatic vein cut by steep to shallow picrolite. peic end fault with subhorizontal striae."	
"399"	"U1601"	"C"	"19"	"R"	"4"	""	"399-U1601C-19R-4"	"0.0"	"59.0"	"109.670"	"109.965"	"110.260"	"109.67"	"109.965"	"110.26"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This section is orthopyroxene-bearing dunite with granular and minor interstitial orthopyroxene."	"Partially to completely serpentinized Opx-bearing dunite."	"Protoganular to prophyroclastic (0° dip) serpentinized harzburgite with locally developed mesh."	
"399"	"U1601"	"C"	"20"	"R"	"1"	""	"399-U1601C-20R-1"	"0.0"	"143.5"	"110.300"	"111.017"	"111.735"	"110.3"	"111.017"	"111.735"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21"	""	"This section is orthopyroxene-bearing dunite grading downward to harzburgite with 20% orthopyroxene and trace chromium spinel at c. 27 cm. "	"Partially to completely serpentinized harzburgite and dunite. The latter is interspersed with hydrothermally altered mafic veins."	"Serpentinized harzburgite with local porphyroclastic fabric and regular to strongly foliated mesh, sub horizontal. Dunite interval with gently dipping mesh and moderately dipping contact.  Cut by subvertical white veins,"	
"399"	"U1601"	"C"	"20"	"R"	"2"	""	"399-U1601C-20R-2"	"0.0"	"93.0"	"111.735"	"112.200"	"112.665"	"111.735"	"112.2"	"112.665"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with about 20 % orthopyroxene and trace clinopyroxene and chromium spinel."	"Partially to completely serpentinized harzburgite and dunite; the latter is interspersed with hydrothermally altered mafic veins."	"Protogranular serpentinized harzburgite with 30°dipping mesh, cut by vertical green veins, horizontal grey vein, and moderately inclined white-green veins."	
"399"	"U1601"	"C"	"20"	"R"	"3"	""	"399-U1601C-20R-3"	"0.0"	"109.0"	"112.665"	"113.210"	"113.755"	"112.665"	"113.21"	"113.755"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is harzburgite with about 20 % orthopyroxene and trace clinopyroxene and chromium spinel grading downward to orthopyroxene-bearing dunite at c. 67 cm."	"Partially to completely serpentinized harzburgite and dunite; the latter is interspersed with hydrothermally altered mafic veins. The bottom of this section contains altered gabbro rubble."	"Serpentinized harzburgite with local weakly foliated mesh (30° dip).  MBIO gabbro rubble has protomylonite fabric.Cut by subhorizontal little white veins, and a sheared white vein."	
"399"	"U1601"	"C"	"21"	"R"	"1"	""	"399-U1601C-21R-1"	"0.0"	"150.0"	"115.200"	"115.950"	"116.700"	"115.2"	"115.95"	"116.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27"	""	"Dunite with about half a percent chromium spinel makes up the top of the section. An altered and deformed medium-grained gabbronorite is present below 69 cm and as a domain at 0-13 cm."	"Partially altered and deformed gabbro cut by hydrothermal veins made of amphibole, chlorite, and prehnite. Hydrothermal alteration is associated with cataclastic deformation at the top of this section (1 to 13cm). The vein density in the cataclastic zone is high."	"Deformed serpentinite and gabbro. 01-14cm vertical contact between protomylonitic gabbro and serpentinite. 14-72cm foliated deformed serpentinite with brittle overprint. 72-109cm gabbro, isotropic, with locally defomred sections (cp foliation). White-green veins cut deformation in deformed gabbro and serpentinized peridotite. "	
"399"	"U1601"	"C"	"22"	"R"	"1"	""	"399-U1601C-22R-1"	"0.0"	"119.0"	"120.000"	"120.595"	"121.190"	"120"	"120.595"	"121.19"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Medium-grained olivine-bearing gabbro with variable grain sizes."	"Variably altered gabbro. Degree of alteration increases downward. Weathering is locally apparent in pieces # 4a, 5, 7. Several types of veins crosscut the gabbro, including amphibole-chlorite veins (that appear to e locally weathered), chlorite veins, quartz veins, and late zeolite veins."	"Isotropic to protomylonitic gabbro with moderately dipping foliation, cut by green to white veins with shallow to steep dips."	
"399"	"U1601"	"C"	"22"	"R"	"2"	""	"399-U1601C-22R-2"	"0.0"	"88.0"	"121.190"	"121.630"	"122.070"	"121.19"	"121.63"	"122.07"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Medium-grained olivine-bearing gabbronorite with variable grain sizes."	"Variably altered gabbro with increasing alteration degree in proximity to a deformed interval. Several types of veins crosscut the gabbro, including amphibole-chlorite veins that cut through chlorite-quartz veins, and late zeolite veins."	"Gabbro showing grain size variation and protomylonitic intervals with moderate dip."	
"399"	"U1601"	"C"	"23"	"R"	"1"	""	"399-U1601C-23R-1"	"0.0"	"133.0"	"124.900"	"125.565"	"126.230"	"124.9"	"125.565"	"126.23"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Highly deformed gabbronorite down to 115 cm. A dunite with trace orthopyroxene and chromium spinel is below."	"Variably altered and deformed gabbro. Degree of alteration increases towards the cataclastic zone, displaying a high vein density."	"Gabbro showing grain size variation cut by sub-vertical mylonitic zone near contact above dunite and serpentinized harzburgite. Section cut by shallow to steep white veins. "	
"399"	"U1601"	"C"	"23"	"R"	"2"	""	"399-U1601C-23R-2"	"0.0"	"132.5"	"126.230"	"126.892"	"127.555"	"126.23"	"126.892"	"127.555"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"The dunite continues from the overlying section, which grades to orthopyroxene-bearing dunite with trace clinopyroxene and chromium spinel at c. 52 cm."	"Highly serpentinized and deformed dunite with brown stained mesh. A magmatic vein is hydrothermally altered. Sulfide locally occurs together with quartz (?) in veins."	"Protogranular to porphyroclastic serpentinized harzburgite with shallow dip and weakly foliated mesh. Dunite at the top of the section with weakly foliated, horizontal mesh.  Cut by green and white veins. "	
"399"	"U1601"	"C"	"24"	"R"	"1"	""	"399-U1601C-24R-1"	"0.0"	"146.0"	"129.700"	"130.430"	"131.160"	"129.7"	"130.43"	"131.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"The upper 52cm is an orthpyroxene-bearing dunite. It is underlain by an olivine-gabbronorite consisting gabbroic and troctolitic domains. The opx in the gabbronorite may have originated in harzburgite. Below 76 cm is an orthopyroxene-bearing dunite."	"Highly serpentinized and deformed dunite with brown stained mesh intruded by a 35cm-thick gabbro layer. The gabbroic layer displays ductile and brittle deformation accompanied with hydrothermal alteration. Its is crosscut by numerous quartz-clays veins."	"Protogranular serpentinized harzburgite with moderately foliated  mesh dipping 20°. Interval of gabbro with modal layering and isotropic sections, cut by protomylonitic deformation and brittle overprint. Cut by green veins and white veins."	
"399"	"U1601"	"C"	"24"	"R"	"2"	""	"399-U1601C-24R-2"	"0.0"	"138.0"	"131.160"	"131.850"	"132.540"	"131.16"	"131.85"	"132.54"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The orthopyroxene-bearing dunite continues from the overlying section."	"Highly serpentinized harzburgite and Opx-bearing dunite crosscut by a hydrothermally altered magmatic vein (130-138cm). A set of grey veins containing sulfides is parallel to the magmatic vein."	"Serpentinized harzburgite with local weak, subhorizontal porphyroclastic foliation, and regular mesh. Multiple vein generations."	
"399"	"U1601"	"C"	"25"	"R"	"1"	""	"399-U1601C-25R-1"	"0.0"	"114.0"	"134.600"	"135.170"	"135.740"	"134.6"	"135.17"	"135.74"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Most of this section is medium-grained gabbronorite. The bottommost piece is coarser grained."	"Variably altered Ol-bearing gabbro. Alteration intensity increases near hydrothermal veins. Slightly weathered next to some veins. Several vein generations cut through the gabbro, including locally weathered amphibole-chlorite veins, quartz with possible former sulfides now orange stained, and late zeolite veins."	"Isotropic, fine to medium grained, with vertical contact defined by grain size variaitons; cut by white veins."	
"399"	"U1601"	"C"	"25"	"R"	"2"	""	"399-U1601C-25R-2"	"0.0"	"125.0"	"135.740"	"136.365"	"136.990"	"135.74"	"136.365"	"136.99"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"The coarse grained gabbronorite continues from the overlying section. Below is a gabbronorite averaging medium-grained, although grain sizes vary significantly."	"Variably altered Ol-bearing gabbro. The background alteration intensity increases near hydrothermal veins. Slightly weathered next to some veins. Several vein generations cut through the gabbro, including amphibole-chlorite veins, veins composed of clays and Fe-oxyhydroxide and an unidentified mineral, and late zeolite veins."	"Isotropic gabbro with grain size variation cut by a single, vertical vein."	
"399"	"U1601"	"C"	"26"	"R"	"1"	""	"399-U1601C-26R-1"	"0.0"	"143.0"	"139.400"	"140.115"	"140.830"	"139.4"	"140.115"	"140.83"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28, 29"	""	"This section is mixed gabbroic and mantle rocks. Most of the upper 45 cm is gabbronorite some bearing olivine, some bearing oxide. Below 45 cm is mostly orthopyroxene-bearing dunite with a domain of olivine gabbro."	"Hydrothermally altered and weathered gabbro and completely serpentinized and partially weathered Opx-bearing dunite."	"Isotropic gabbro with mylonite above serpentinzed protogranular harzburgite and strongly foliated (subhorizontal) to regular mesh cut by moderate dip white vein."	
"399"	"U1601"	"C"	"27"	"R"	"1"	""	"399-U1601C-27R-1"	"0.0"	"97.0"	"144.300"	"144.785"	"145.270"	"144.3"	"144.785"	"145.27"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is mostly dunite (0-27.5 cm and below 64 cm) and harzburgite with about 10 % orthopyroxene. highly altered gabbronorites are present from 14-22 cm and below 83 cm."	"Mostly serpentinized and weathered harzburgite with minor hydrothermally altered gabbro (top of the section). Sparse chrysotile veins. Some of the serpentine-magnetite veins are oxidized to hematite and goethite."	"Weak to strongly foliated porphyroclastic to protomylonitic serpentinized harzburgite (steep dip), with no to strongly developed mesh, with  well developed sheared gabbo veins (contact and fabric both steeply dipping)."	
"399"	"U1601"	"C"	"28"	"R"	"1"	""	"399-U1601C-28R-1"	"0.0"	"127.0"	"149.100"	"149.735"	"150.370"	"149.1"	"149.735"	"150.37"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section has intermingled orthopyroxene-bearing dunite and harzburgite with medium-grained gabbronorite (intervals: 15-56 cm and 82-100 cm). The peridotites all have trace spinel."	"Mostly serpentinized and weathered Opx-bearing dunite with minor hydrothermally altered gabbro (0 to 16 and 56 to 82 cm). Gabbro is crosscut by amphibole, quartz-chlorite and zeolite veins. Chrysotile veins in the dunite are weathered."	"Serpentinized harzburgite cut by intervals of isotropic gabbro. Serpentine has strong foliated (30° dip) to unfoliated mesh. Shallow to vertical green, white, and red veins, including one with vertical slickenfibers"	
"399"	"U1601"	"C"	"28"	"R"	"2"	""	"399-U1601C-28R-2"	"0.0"	"88.0"	"150.600"	"151.040"	"151.480"	"150.6"	"151.04"	"151.48"	""	"1, 2, 3, 4, 5, 6"	""	"Orthopyroxene-bearing dunite and harzburgite with trace spinel. The orthopyroxene is mostly granular."	"Completely serpentinized and highly weathered Opx-bearing dunite and harzburgite. Mesh after olivine is brown stained. Bastite appears less weathered than mesh."	"Protogranular serpentinized harzburgite, with unfoliated to weakly foliated mesh (dip 20°). White veins, inclined to steep."	
"399"	"U1601"	"C"	"29"	"R"	"1"	""	"399-U1601C-29R-1"	"0.0"	"104.0"	"154.000"	"154.520"	"155.040"	"154"	"154.52"	"155.04"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The upper 37.5 cm is orthopyroxene-bearing dunite with mostly granular orthopyroxene. Below is mostly harzburgite with about 12% granular and interstitial orthopyroxene.  Highly-altered gabbronorite veins cut the upper 32 cm of the section and at c. 76 cm."	"Highly to completely serpentinized and highly weathered harzburgite crosscut by 4 magmatic veins. Mesh after olivine is brown stained. Magmatic veins are hydrothermally altered to chlorite, amphibole, and possibly prehnite, epidote, and secondary plagioclase."	"Protogranular serpentinized harzburgite with localized, patchy mesh, cut by cut by subhorizontal to inclined magmatic veins, overprinted by white veins, green veins."	
"399"	"U1601"	"C"	"29"	"R"	"2"	""	"399-U1601C-29R-2"	"0.0"	"123.0"	"155.260"	"155.875"	"156.490"	"155.26"	"155.875"	"156.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with about 15% orthopyroxene down to 57.5 cm, underlain by orthopyroxene-bearing dunite cut by highly altered cm-scale gabbronorite veins at c. 44, 62, and 86 cm."	"Highly to completely serpentinized and highly weathered harzburgite and Opx-bearing dunite crosscut by 2 magmatic veins. Mesh after olivine is brown stained. Magmatic veins are hydrothermally altered to chlorite, amphibole, and possibly prehnite, epidote, and secondary plagioclase. Bastite appears less weathered than mesh."	"Protogranular serpentinized harzburgite with localized, patchy mesh, cut by white veins; oxidized colors. "	
"399"	"U1601"	"C"	"30"	"R"	"1"	""	"399-U1601C-30R-1"	"0.0"	"121.0"	"158.800"	"159.405"	"160.010"	"158.8"	"159.405"	"160.01"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Dunite above harzburgite. The dunite has trace clinopyroxene, plagioclase, and spinel. Contains diffuse gabbro veins at 114-145 cm."	"Highly to completely serpentinized and highly weathered Opx-bearing dunite crosscut by altered magmatic veins. Mesh after olivine is brown stained. Bastite is also slightly oxidized. Top of the section is composed of diabase (4 cm). Magmatic veins are hydrothermally overprinted to chlorite, amphibole, possibly prehnite, and secondary plagioclase."	"Protogranular, serpentinized harzburgite with red oxidized colors and a patchy unfoliated mesh, and a dunite interval with moderate dip contact, all cut by magmatic vein and later white, and white-green veins."	
"399"	"U1601"	"C"	"30"	"R"	"2"	""	"399-U1601C-30R-2"	"0.0"	"116.0"	"160.250"	"160.830"	"161.410"	"160.25"	"160.83"	"161.41"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Orthopyroxene-bearing dunite to harzburgite with orthopyroxene proportions increasing down section.  Contains diffuse gabbro patches at 13-35 cm."	"Highly to completely serpentinized and highly weathered Opx-bearing dunite crosscut by altered magmatic veins. Mesh after olivine is brown stained. Bastite is also slightly oxidized. Magmatic veins are hydrothermally overprinted to chlorite, amphibole, possibly prehnite, and secondary plagioclase."	"Protogranular to weakly porphyroclastic serpentinized harzburgite (subhorizontal mantle fabric), with unfoliated mesh. Cut by magmatic veins, in turn cut by white veins."	
"399"	"U1601"	"C"	"31"	"R"	"1"	""	"399-U1601C-31R-1"	"0.0"	"121.0"	"163.700"	"164.305"	"164.910"	"163.7"	"164.305"	"164.91"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"Orthopyroxene-bearing dunite above harzburgite, both with trace spinel."	"Highly to completely serpentinized and variably weathered Opx-bearing dunite and harzburgite. Mesh after olivine is locally brown stained suggesting oxidation. Downhole, mesh texture appears green and black while it is black and brown near the top of this section. Late carbonate veining (one single vein)."	"Protogranular serpentinized harzburgite with patchy unfoliated mesh, cut by white veins. Less oxidized colors than above (mostly black)."	
"399"	"U1601"	"C"	"31"	"R"	"2"	""	"399-U1601C-31R-2"	"0.0"	"118.0"	"165.200"	"165.790"	"166.380"	"165.2"	"165.79"	"166.38"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The upper 10 cm is harzburgite. Below is dunite to orthopyroxene- bearing dunite above harzburgite. Spinel is present throughout, but is particularly concentrated in the dunite. Orthopyroxene distribution is generally uneven."	"Highly to completely serpentinized and variably weathered Opx-bearing dunite and harzburgite. Mesh after olivine is locally brown stained suggesting oxidation. Late carbonate veining (one single vein)."	"Serpentinized harzburgite with thin dunite interval hosting aligned spinel layer subparallel to the moderately dipping cotact. Harzburgite shows  protogranular to weakly foliated porphyroclastic foliation, subhorizontal and patchy strongly foliated (horizontal) to unfoliated mesh. Cut by horizontal to moderately inclined little white veins."	
"399"	"U1601"	"C"	"31"	"R"	"3"	""	"399-U1601C-31R-3"	"0.0"	"56.0"	"166.520"	"166.800"	"167.080"	"166.52"	"166.8"	"167.08"	""	"1, 2, 3, 4, 5, 6"	""	"Orthopyroxene-bearing dunite above a coarse-grained gabbro unit. The dunite is cut by a few altered gabbroic veins."	"Highly to completely serpentinized and variably weathered Opx-bearing dunite crosscut by altered magmatic vein. Hydrothermally altered gabbro at the bottom of the section. Mesh after olivine is locally brown stained suggesting oxidation. The magmatic vein is overprinted by chlorite, amphibole, and secondary plagioclase. Prehnite veins crosscut the altered gabbro."	"Protogranular serpentinized harzburgite with no mesh, cut by isotropic, fractured gabbro, in turn cut by red oxidized, multiple cross cutting veins."	
"399"	"U1601"	"C"	"32"	"R"	"1"	""	"399-U1601C-32R-1"	"0.0"	"116.0"	"168.500"	"169.080"	"169.660"	"168.5"	"169.08"	"169.66"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Harzburgite from 0-16 cm, underlain by olivine-bearing gabbronorite. Olivine gabbro is below 117 cm."	"Gabbro altered to greenstone and serpentinized harzburgite. The serpentinized harzburgite is crosscut by a network of partly oxidized chrysotile veins. Quartz-carbonate and chlorite-prehnite veins crosscut the altered gabbro."	"Thin interval of serpentinized harzburgite, above thick section of gabbro. Gabbro has protomylonitic to mylonitic intervals with 20 deg dip. Undeformed gabbro is isotropic with moderate dip (45°) grainsize layering, cut by qtz veins and magmatic veins."	
"399"	"U1601"	"C"	"32"	"R"	"2"	""	"399-U1601C-32R-2"	"0.0"	"123.0"	"170.000"	"170.615"	"171.230"	"170"	"170.615"	"171.23"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Olivine gabbro unit with significant variations in grain size, mode and texture on a small scale. Rock types range from gabbro to troctolite, which are intermingled down to the cm-scale."	"Hydrothermally altered gabbro cut by carbonate veins. Chlorite and amphibole replace plagioclase and clinopyroxene, respectively."	"Isotropic gabbro with grain size variations. Cut by white and dark green vein."	
"399"	"U1601"	"C"	"33"	"R"	"1"	""	"399-U1601C-33R-1"	"0.0"	"31.0"	"173.400"	"173.555"	"173.710"	"173.4"	"173.555"	"173.71"	""	"1, 2, 3, 4"	""	"Opx-bearing dunite. Gabbroic impregation in top & bottom pieces."	"Highly altered brown rock, protolith is uncertain. Brown stained. Contains disseminated sulfides. Cut by sulfides veins and white massive to fibrous veins (serpentine?)"	"Isotropic gabbro with grainsize variations above protogranular, serpentinzed harzburgite, with regular mesh; cut by magmatic vein, then dark veins and later white veins.  Greenschist static alteration, cut by white veins and dark green vein."	
"399"	"U1601"	"C"	"33"	"R"	"1"	""	"399-U1601C-33R-1"	"0.0"	"150.0"	"173.400"	"174.150"	"174.900"	"173.4"	"174.15"	"174.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Opx-bearing dunite with trace spinel. Gabbroic impregation in top & bottom pieces."	"Highly altered brown rock, protolith is uncertain. Brown stained. Contains disseminated sulfides. Crosscut by sulfides veins and picrolite-like veins."	"Isotropic gabbro with grainsize variations above protogranular, serpentinzed harzburgite, with regular mesh; cut by magmatic vein, then dark veins and later white veins.  Greenschist static alteration, cut by white veins and dark green vein."	
"399"	"U1601"	"C"	"33"	"R"	"2"	""	"399-U1601C-33R-2"	"0.0"	"138.0"	"174.905"	"175.595"	"176.285"	"174.905"	"175.595"	"176.285"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Interleaved orthopyroxene bearing dunite and harzburgite, both with trace spinel"	"Partially serpentinized harzburgite and Opx-bearing dunite. Several vein types including mesh and chrysotile veins."	"Strongly foliated porphyroclastic serpentinized harzburgite (mantle fabric dips 15-40°), cut by green and white veins."	
"399"	"U1601"	"C"	"33"	"R"	"3"	""	"399-U1601C-33R-3"	"0.0"	"52.0"	"176.405"	"176.665"	"176.925"	"176.405"	"176.665"	"176.925"	""	"1, 2, 3, 4, 5"	""	"Relatively coarse grained harzburgite with c. 20% orthopyroxene and trace spinel."	"Partially serpentinized harzburgite and Opx-bearing dunite. Several vein types including mesh, chrysotile, and late serpentine-carbonate veins."	" Protogranular to weakly porphyroclastic serpentinized harzburgite with moderately foliated serpentiine mesh (5°), cut by moderately dipping veins. "	
"399"	"U1601"	"C"	"34"	"R"	"1"	""	"399-U1601C-34R-1"	"0.0"	"100.0"	"178.200"	"178.700"	"179.200"	"178.2"	"178.7"	"179.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Interspersed serpentinized peridotites and gabbroic veins. Most of the section is harzburgite. Gabbroic veins range from gabbro to olivine-bearing gabbro with variable grain sizes."	"Opx-bearing dunite cut by magmatic vein that is hydrothermally altered. Altered gabbro at the top of the section. Vein types in the dunite include serpentine-magnetite, chrysotile, and late serpentine-carbonate veins. The magmatic vein (gabbroic) is crosscut by quartz and chlorite veins."	"Protogranular serpentinized harzburgite with weakly foliated mesh (10 ° dip), cut by magmatic veins, and white veins. One thin interval of isotropic gabbro."	
"399"	"U1601"	"C"	"34"	"R"	"2"	""	"399-U1601C-34R-2"	"0.0"	"50.0"	"179.400"	"179.650"	"179.900"	"179.4"	"179.65"	"179.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with minimal orthopyroxene. About 30 % of section consists of olivine gabbro veins and patches."	"Strongly serpentinized and weathered Opx-bearing dunite, cut by hydrothermally overprinted magmatic vein. Serpentine-magnetite veins are abundant. Chrysotile and late serpentine-carbonate veins cut the serpentinite and the hydrothermally altered magmatic veins."	"Small pieces of serpentinized harzburgite cut by magmatic veins and white veins, no orientated pieces."	
"399"	"U1601"	"C"	"35"	"R"	"1"	""	"399-U1601C-35R-1"	"0.0"	"150.0"	"183.100"	"183.850"	"184.600"	"183.1"	"183.85"	"184.6"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26"	""	"Hybrid rock with two domains: (1) poikilitic micro gabbro domain composed of coarse-grained cpx oikocrysts enclosing microcrystalline plagioclase. (2) Medium-grained granular troctolite domain with grain size variation on a 10s of centimeter scale. In this section, domains are generally discrete, but hybridization does occur between them. Trace sulfide."	"Highly altered gabbro (greenstone) with variably altered troctolitic domains in pieces in # 9, 15, and 16. The gabbro and troctolite are cut by quartz-pyrite veins. The latter seems to be locally altered to clays. Clay veins also cut through the gabbro. A network of thin zeolite veins is present throughout the section."	"Isotropic gabbro with subvertical modal and grain size contacts, cut by shallow to moderately dipping black, green, and white veins."	
"399"	"U1601"	"C"	"35"	"R"	"2"	""	"399-U1601C-35R-2"	"0.0"	"150.0"	"184.600"	"185.350"	"186.100"	"184.6"	"185.35"	"186.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Hybrid rock with two domains: (1) poikilitic micro gabbro domain composed of coarse-grained cpx oikocrysts enclosing microcrystalline plagioclase. (2) Medium-grained granular troctolite domain with grain size variation on a 10s of centimeter scale. In this section, hybridization has proceeded to the point that some pieces (e.g., 8, 15) are hybrid olivine gabbro. Trace sulfide."	"Highly altered gabbro (greenstone) with variably altered troctolitic domains. In pieces # 11 to 13 the extent of alteration is highest near veins and olivine is absent. The gabbro is cut by several vein types including quartz-amphibole veins, quartz-pyrite veins (locally overprinted by clays), clay veins, and a network of zeolite veins. The replacement of former sulfides into Fe-oxyhydroxides in quartz-pyrite veins suggests oxidation."	"Isotropic gabbro with modal and grain size contacts (shallow to moderate dip), cut by white to orange shallow to moderately dipping veins."	
"399"	"U1601"	"C"	"36"	"R"	"1"	""	"399-U1601C-36R-1"	"0.0"	"143.0"	"187.900"	"188.615"	"189.330"	"187.9"	"188.615"	"189.33"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Hybrid rock with poikilitic gabbro and troctolitic domains continued from previous section, underlain by an interval of medium-grained olivine gabbro. Trace sulfide."	"Highly altered gabbro (greenstone) with variably altered troctolitic domains. In pieces # 5 to 10, the extent of alteration is highest near veins and olivine completely altered. The gabbro is cut by several vein types including quartz-pyrite veins (locally overprinted by clays) and a network of zeolite veins. The replacement of former sulfides into Fe-oxyhydroxides in quartz-pyrite veins suggests oxidation."	"Isotropic gabbro with modal and grain size contacts with shallow to moderate dips, cut by black white vuggy shallowly dipping veins."	
"399"	"U1601"	"C"	"36"	"R"	"2"	""	"399-U1601C-36R-2"	"0.0"	"110.0"	"189.330"	"189.880"	"190.430"	"189.33"	"189.88"	"190.43"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Medium-grained olivine gabbro continuous from previous section. Piece #11 contains little olivine."	"Highly altered olivine gabbro (greenstone). Next to the veins, the degree of alteration increases and olivine is almost completely altered. Preferential weathering along fractures cutting through some pieces can be observed. The gabbro is cut by several vein types including quartz and minor amphibole veins locally overprinted by clay formation, clay veins, and a network of zeolite veins."	"Isotropic gabbro with modal and grainsize domains. cut by sub-vertical green veins."	
"399"	"U1601"	"C"	"37"	"R"	"1"	""	"399-U1601C-37R-1"	"0.0"	"125.0"	"192.800"	"193.425"	"194.050"	"192.8"	"193.425"	"194.05"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Medium-grained, granular olivine gabbro with variable grain size; continuation of previous section."	"Variably altered and weathered olivine gabbro. Preferential oxidation along fractures cutting through some pieces. Several vein types can be recognized, including amphibole veins, quartz and brown-stained mineral veins, and zeolite-chlorite veins (latest generation)."	"Isotropic gabbro with grain size variation, with localized brittle deformation. Cut by quartz and black veins with shallow to moderately dipping."	
"399"	"U1601"	"C"	"37"	"R"	"2"	""	"399-U1601C-37R-2"	"0.0"	"92.5"	"194.050"	"194.512"	"194.975"	"194.05"	"194.512"	"194.975"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Complex multi-component olivine gabbro. Patches are coarser and trend towards troctolitic composition, these occur as irregular zones in a finer-grained cpx-rich olivine gabbro. Resembles section 35."	"Variably altered and weathered olivine gabbro. Preferential oxidation at some piece ends. Locally the gabbro is altered to greenstone. Several vein types are present, including amphibole, chlorite, zeolite-chlorite, and quartz-sulfide veins. In fine-grained microgabbro and gabbro is a highly altered amphibole-rich zone."	"Isotropic gabbro with irregular grain size domains and greenschist overprint. Cut by green and dark green veins with moderate dip."	
"399"	"U1601"	"C"	"37"	"R"	"3"	""	"399-U1601C-37R-3"	"0.0"	"95.5"	"194.975"	"195.452"	"195.930"	"194.975"	"195.452"	"195.93"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Change in grain sizes and modes from above sections. Here, the rock is a medium-grained gabbronorite, which is coarser than the overlying olivine gabbro. The basal 31 cm is an orthopyroxene-bearing dunite."	"Variably altered olivine-bearing gabbro. Amphibolite at the bottom of the section (55.5-92.5 cm) and amphibolite rubble at the top of the section (0-4.5 cm). Different vein types are made of prehnite-chlorite, quartz-chlorite, and zeolite veins. Prehnite and chlorite are present at the contact between amphibolite and the altered olivine-bearing gabbro."	"Isotropic, coarse grained gabbro, cut by a sheared vein. Serpentinized harburgite interval at base of section."	
"399"	"U1601"	"C"	"38"	"R"	"1"	""	"399-U1601C-38R-1"	"0.0"	"150.0"	"197.600"	"198.350"	"199.100"	"197.6"	"198.299"	"198.999"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The top bin has what appears to be an accidental pebble of olivine-bearing gabbro. The rest of the section is mostly harzburgite with c. 3 % gabbro in veins ranging in width from 2 to 15 mm."	"Highly serpentinized and weathered harzburgite cut by hydrothermally altered magmatic vein. Altered gabbro pebble. Vein types include serpentine-magnetite veins and composite picrolite-carbonate veins, as well as late carbonate-sulfide-serpentine veins that locally cut picrolite veins."	"Protogranular serpentinized harzburgite with no mesh. Small interval of isotropic gabbro at top. Cut by several generations of veins. Fault surface (30° dip) with normal sense slickenfibres, on green-white vein."	
"399"	"U1601"	"C"	"38"	"R"	"2"	""	"399-U1601C-38R-2"	"0.0"	"132.0"	"199.100"	"199.760"	"200.420"	"198.999"	"199.614"	"200.229"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with approximately 15 % orthopyroxene and trace spinel."	"Highly serpentinized and weathered Opx-bearing dunite cut by hydrothermally altered magmatic vein. Vein types include serpentine-magnetite, composite picrolite-carbonate veins, and late carbonate-sulfides-serpentine veins that locally cut picrolite veins."	"Protogranular serpentinized harzburgite with weakly foliated to no mesh, cut by moderately dipping white veins."	
"399"	"U1601"	"C"	"38"	"R"	"3"	""	"399-U1601C-38R-3"	"0.0"	"138.5"	"200.420"	"201.113"	"201.805"	"200.229"	"200.873"	"201.517"	""	"1"	""	"Harzburgite with approximately 15 % orthopyroxene and trace spinel. Cpx may be present."	"Highly serpentinized and partially weathered harzburgite. Vein types include serpentine-magnetite veins, picrolite veins, and late composite picrolite-carbonate veins. It seems likely that carbonates reopened the former picrolite veins."	"Weakly foliated porphyroclastic serpentinized harzburgite (15 deg) with weak mesh foliation. Cut by moderately dipping white veins and a magmatic vein."	
"399"	"U1601"	"C"	"38"	"R"	"4"	""	"399-U1601C-38R-4"	"0.0"	"105.0"	"201.805"	"202.330"	"202.855"	"201.521"	"202.011"	"202.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with about 10 % olivine gabbronorite. The reaction front between the gabbronorite and harzburgite is troctolitic."	"Highly serpentinized and weathered harzburgite cut by hydrothermally overprinted magmatic veins. The latter is made of chlorite and amphibole after plagioclase and clinopyroxene, respectively. Primary igneous mineral relicts are present. Several vein types cut through the peridotite including serpentine-magnetite, picrolite, and late composite picrolite-carbonate veins. It seems likely that carbonates reopened the former picrolite veins. Picrolite veins also cut through the hydrothermal magmatic veins."	"Protogranular serpentinized harzburgite with a regular mesh, cut by moderately to steeply dipping magmatic vein and moderately dipping white veins."	
"399"	"U1601"	"C"	"39"	"R"	"1"	""	"399-U1601C-39R-1"	"0.0"	"149.0"	"202.500"	"203.245"	"203.990"	"202.5"	"203.243"	"203.985"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Harzburgite with interspersed gabbro.  The gabbro between 32 and 85 cm is coarse grained to pegmatitic amd olivine-bearing. The cm-wide reaction boundary against the harzburgite is troctolitic. A 4 mm-wide olivine gabbro vein also is present. "	"Highly serpentinized and partially weathered harzburgite cut by hydrothermally overprinted magmatic vein. Altered pegmatitic gabbro. Bastite close to the gabbro contact is dark. Several vein types cut through the serpentinized peridotite including mesh, chrysotile-picrolite, and late carbonate and clay veins. Picrolite veins also cut through the hydrothermal magmatic veins. The altered gabbro is crosscut by prehnite-chlorite-carbonate veins."	"Protogranular to weakly foliated porphyroclastic (5° dipping mantle fabric) serpentinized harzburgite with no to moderately foliated mesh. Steeply dipping interval (irregular contact against harzburgite) of altered gabbro cut by white-green, gently dipping veins."	
"399"	"U1601"	"C"	"39"	"R"	"2"	""	"399-U1601C-39R-2"	"0.0"	"102.0"	"203.990"	"204.500"	"205.010"	"203.985"	"204.494"	"205.002"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with about 20% orthopyroxene and trace spinel."	"Highly serpentinized harzburgite cut by serpentine-magnetite, chlorite-amphibole, and late carbonate veins."	"Porphyroclastic serpentinized harzburgite (gently dipping mantle fabric)  with patchy to weak, subhorizontal mesh. Cut by steep to moderately dipping white veins."	
"399"	"U1601"	"C"	"39"	"R"	"3"	""	"399-U1601C-39R-3"	"0.0"	"103.0"	"205.010"	"205.525"	"206.040"	"205.002"	"205.516"	"206.029"	""	"1"	""	"Harzburgite with about 20% orthopyroxene and trace spinel."	"Highly serpentinized harzburgite crosscut by serpentine-magnetite, chlorite, chrysotile, and late carbonate veins."	"Weakly foliated porphyroclastic serpentinized harzburgite hostng a weak mesh (5° dip). Cut by white veins parallel to mesh, and magmatic, white-grey and black-white veins."	
"399"	"U1601"	"C"	"39"	"R"	"4"	""	"399-U1601C-39R-4"	"0.0"	"127.5"	"206.040"	"206.678"	"207.315"	"206.029"	"206.667"	"207.304"	""	"1, 2, 3"	""	"Harzburgite with about 20% orthopyroxene and trace spinel."	"Highly serpentinized harzburgite crosscut by serpentine-magnetite, chlorite, chrysotile, and late carbonate-sulfide-serpentine veins. It is likely that carbonates reopened the former serpentine veins."	"Weakly foliated porphyroclastic serpentinized harzburgite with weak to strong mesh (15° dip). Cut by white veins parallel to mesh, and cross-cutting magmatic, and white-grey veins."	
"399"	"U1601"	"C"	"40"	"R"	"1"	""	"399-U1601C-40R-1"	"0.0"	"62.0"	"207.300"	"207.610"	"207.920"	"207.3"	"207.61"	"207.92"	""	"1"	""	"Harzburgite with trace spinel, continuous from previous section. "	"Highly serpentinized harzburgite, cut by diffuse hydrothermally altered magmatic vein. The latter is made of chlorite, possibly secondary plagioclase, amphibole, and an unidentified brown mineral. The serpentinized harzburgite is crosscut by hydrothermal veins including serpentine-magnetite, chlorite, chrysotile, and late carbonate veins."	"Protogranular serpentinized harzburgite with horizontal weak mesh cut by steeply dipping white vein, a moderate dip green vein and horizontal little white veins."	
"399"	"U1601"	"C"	"40"	"R"	"2"	""	"399-U1601C-40R-2"	"0.0"	"143.0"	"207.920"	"208.635"	"209.350"	"207.92"	"208.635"	"209.35"	""	"1"	""	"Harzburgite with trace spinel, continuous from previous section. Has a diffuse reaction zone that contains low modal opx close to the contacts with a gabbro vein at 7.5-14 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. The magmatic vein is made of chlorite and amphibole after plagioclase and clinopyroxene, respectively. It also contains opaque minerals and is crosscut by massive "picrolite-like" veins. The serpentinized harzburgite is crosscut by hydrothermal veins including serpentine-magnetite, picrolite, and chrysotile veins."	"Protogranular serpentinized harzburgite with unfoliated mesh, and one magmatic veins cut the moderately fipping green and white veins."	
"399"	"U1601"	"C"	"40"	"R"	"3"	""	"399-U1601C-40R-3"	"0.0"	"143.0"	"209.350"	"210.065"	"210.780"	"209.35"	"210.065"	"210.78"	""	"1"	""	"Continued harzburgite with trace spinel."	"Highly serpentinized harzburgite, cut by hydrothermally altered small magmatic veins. The latter is made of amphibole and chlorite and is cut by chrysotile veins. The serpentinized harzburgite is crosscut by hydrothermal veins including serpentine-magnetite, fibrous chrysotile, and late carbonate veins. The latter veins occur at the end of the pieces."	"Weakly foliated pophyroclastic serpentinized harzburgite (30° changing to 20° gradually down section); regular mesh. Cut by thick white veins with 50°dip."	
"399"	"U1601"	"C"	"40"	"R"	"4"	""	"399-U1601C-40R-4"	"0.0"	"97.0"	"210.780"	"211.265"	"211.750"	"210.78"	"211.265"	"211.75"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"12.5 cm of dunite above, in sequence, coarse-grained olivine-bearing gabbro, olivine gabbro with variable textures and grain sizes, and orthopyroxene-bearing dunite. Trace spinel is present in the peridotites."	"Highly altered gabbro and serpentinized dunite/troctolite. In the altered gabbro, amphibole and chlorite form after clinopyroxene and plagioclase, respectively. The serpentinized dunite/troctolite contains mesh and is crosscut by chrysotile veins. A network of zeolite veins is present throughout the altered gabbro."	"Thin dunite interval above pyroxenite and gabbro with a horizontal contact.  Gabbro is cut by horizontal green and white veins."	
"399"	"U1601"	"C"	"41"	"R"	"1"	""	"399-U1601C-41R-1"	"0.0"	"145.0"	"212.200"	"212.925"	"213.650"	"212.2"	"212.925"	"213.65"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"Orthopyroxene-bearing dunite with central gabbroic zone consisting of veins with varying thicknesses and textures. Gabbroic rock types range from olivine-bearing gabbro to olivine gabbronorite. The border between the gabbro and dunite is troctolitic."	"Highly altered coarse-grained to pegmatitic gabbro altered to chlorite and amphibole after plagioclase and clinopyroxene, respectively. Strongly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein. The latter is made of secondary plagioclase, chlorite, amphibole, and chlorite."	"Protogranular serpentinized harzburgite with regular mesh intruded isotropic gabbro (shallow to moderate dip contacts). Cut by a moderate dip magmatic veins, land younger pictolite veins."	
"399"	"U1601"	"C"	"41"	"R"	"2"	""	"399-U1601C-41R-2"	"0.0"	"150.0"	"213.650"	"214.400"	"215.150"	"213.65"	"214.4"	"215.15"	""	"1, 2, 3, 4"	""	"Harzburgite with a relatively high proportion of orthopyroxene (c. 25%) and trace spinel. The uppermost piece is cut by a medium-grained gabbro vein."	"Highly serpentinized harzburgite cut by serpentine-magnetite, fibrous chrysotile, and late composite carbonate-sulfide-serpentine veins."	"Protogranular serpentinized harzburgite with moderately foliated mesh (30° dip). Thick white veins parallel to mesh."	
"399"	"U1601"	"C"	"41"	"R"	"3"	""	"399-U1601C-41R-3"	"0.0"	"103.0"	"215.150"	"215.665"	"216.180"	"215.15"	"215.665"	"216.18"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Olivine bearing dunite above harzburgite with intervening gabbronorite. Olivine is included in the gabbronorite near the contact with the serpentinized peridotites. A 2mm-wide altered gabbroic vein is present towards the base of the section."	"Highly serpentinized harzburgite, Opx-bearing dunite, and altered gabbro. The serpentinized peridotite is cut by one hydrothermally altered magmatic vein made of secondary plagioclase, chlorite, prehnite, and amphibole. Serpentine-magnetite, amphibole, chlorite, and late fibrous chrysotile veins occur in this section."	"Protogranular serpentinized harzburgite with moderate to weak mesh foliation (20-25°dip), and isotropic gabbro interval. Moderately dipping magmatic vein cross cut by white green veins."	
"399"	"U1601"	"C"	"41"	"R"	"4"	""	"399-U1601C-41R-4"	"0.0"	"57.5"	"216.180"	"216.468"	"216.755"	"216.18"	"216.468"	"216.755"	""	"1"	""	"Harzburgite with a relatively high proportion of orthopyroxene (c. 25%) and trace spinel. Millimeter-scale gabbroic veins crosscut at 22 cm."	"Highly serpentinized harzburgite cut by three hydrothermally altered magmatic veinlets composed of secondary plagioclase, chlorite, prehnite, and amphibole. Several types of veins cut the serpentinized peridotite including serpentine-magnetite, fibrous chrysotile, and late composite carbonate-serpentine veins. Carbonate-serpentine veins contain clasts of the host rock."	"Serpentinized harzburgite, with subhorizontal weak porphyroclastic foliation and regular mesh. Cut by steep white vein, moderate dip grey-white vein and subhorizontal little white veins."	
"399"	"U1601"	"C"	"42"	"R"	"1"	""	"399-U1601C-42R-1"	"0.0"	"145.0"	"217.000"	"217.725"	"218.450"	"217"	"217.707"	"218.413"	""	"1, 2, 3"	""	"Harzburgite with c. 20% opx and trace spinel and cpx. The top-most piece is a pebble of highly altered gabbro."	"Highly serpentinized harzburgite cut by three hydrothermally altered magmatic veinlets made of secondary plagioclase, chlorite, prehnite, and amphibole. Serpentine-magnetite fibrous chrysotile, and chlorite-opaque mineral-white unidentified mineral veins occur in this section."	"Protogranular serpentinized harzburgite with unfoliated mesh, cut by moderate dip magmatic veins and subhorizontal little white veins."	
"399"	"U1601"	"C"	"42"	"R"	"2"	""	"399-U1601C-42R-2"	"0.0"	"123.0"	"218.450"	"219.065"	"219.680"	"218.413"	"219.012"	"219.611"	""	"1"	""	"Harzburgite with approximately 22% orthopyroxene and trace spinel and cpx. "	"Highly serpentinized harzburgite cut by mesh and fibrous chrysotile veins."	"Protogranular serpentinized harzburgite with patchy regual mesh and little white veins(20° dip). "	
"399"	"U1601"	"C"	"42"	"R"	"3"	""	"399-U1601C-42R-3"	"0.0"	"102.0"	"219.680"	"220.190"	"220.700"	"219.611"	"220.108"	"220.605"	""	"1, 2"	""	"Harzburgite with approximately 25% orthopyroxene and trace spinel and cpx. "	"Highly serpentinized harzburgite cut by mesh and fibrous chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by two moderately diping magmatic veins, and little white veins (15° dip)."	
"399"	"U1601"	"C"	"42"	"R"	"4"	""	"399-U1601C-42R-4"	"0.0"	"133.0"	"220.700"	"221.365"	"222.030"	"220.605"	"221.252"	"221.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with c. 15% orthopyroxene and trace spinel. Contains scattered veins of highly altered gabbroic material (gabbronorite?). "	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins. The latter are made of secondary plagioclase, chlorite, prehnite and amphibole and are crosscut by massive picrolite veins. Several type of veins cut through the serpentinized peridotites including serpentine-magnetite, fibrous chrysotile, and picrolite veins."	"Protogranular serpentinized harzburgite with weakly foliated mesh (10° dip). Cut by multiple magmatic veins (moderate dip), cut by picrolite veins."	
"399"	"U1601"	"C"	"43"	"R"	"1"	""	"399-U1601C-43R-1"	"0.0"	"112.0"	"221.900"	"222.460"	"223.020"	"221.9"	"222.436"	"222.973"	""	"1, 1, 2, 3, 4"	""	"Harzburgite with relatively low orthopyroxene content (12-15%) and trace spinel; cut by several highly altered gabbroic veins. The thickest vein is at about 57 cm. It has a variable  composition and is associated with an interval of orthopyroxene-bearing dunite."	"Highly serpentinized harzburgite and black rock containing plagioclase and black mineral (amphibolite or serpentinized troctolite?) cut by hydrothermally altered magmatic veins composed of secondary plagioclase, chlorite, prehnite, and amphibole cut by picrolite veins. In addition, fibrous chrysotile and late massive clay veins are present."	"Protogranular serpentinized harzburgite with regular mesh. Dunite interval with moderately dipping upper contact, cut by shallow to moderate dip magmatic veins and subhorizontal little white veins."	
"399"	"U1601"	"C"	"43"	"R"	"2"	""	"399-U1601C-43R-2"	"0.0"	"146.0"	"223.020"	"223.750"	"224.480"	"222.973"	"223.673"	"224.372"	""	"1, 2, 3, 4"	""	"Harzburgite with trace clinopyroxene and spinel. Contains a few scattered 1-2 mm gabbro veins. Some are bounded by cm-scale dunitic channels"	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of secondary plagioclase, chlorite, prehnite and amphibole cut by picrolite and fibrous chrysotile veins. In addition, fibrous chrysotile and massive dark-haloed picrolite veins are present in this section."	"Protogranular serpentinized harzburgite with regular mesh. Magmatic veins with moderate dip, cut by white, green, and black veins have moderate dips."	
"399"	"U1601"	"C"	"43"	"R"	"3"	""	"399-U1601C-43R-3"	"0.0"	"83.0"	"224.480"	"224.895"	"225.310"	"224.372"	"224.769"	"225.167"	""	"1"	""	"Harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite cut by discrete hydrothermally altered magmatic veins. The latter are made of secondary plagioclase, chlorite, prehnite, amphibole, and one pink mineral. Magmatic veins are croscut by massive picrolite veins. Several type of veins cut through the serpentinized peridotite including serpentine-magnetite, fibrous chrysotile, and massive dark-haloed picrolite veins."	"Serpentinized harzburgite with regular mesh.  Cut by moderately dipping magmatic vein, moderately dipping white, green, and black veins."	
"399"	"U1601"	"C"	"43"	"R"	"4"	""	"399-U1601C-43R-4"	"0.0"	"113.0"	"225.310"	"225.875"	"226.440"	"225.167"	"225.708"	"226.25"	""	"1, 2"	""	"Harzburgite with trace clinopyroxene and spinel. One 2-cm scale dunite channel at c. 33 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Several types of veins cut through the serpentinized peridotite including mesh, serpentine-magnetite veins, fibrous chrysotile, and late clay veins. The latter possibly overprint former magmatic veins. Serpentine-magnetite veins are crosscut by chrysotile and clay veins."	"Protogranular serpentinized harzburgite with moderately foliated mesh and parallel little white veins (15° dip). Cut by multiple veins with steep to moderate dip."	
"399"	"U1601"	"C"	"43"	"R"	"5"	""	"399-U1601C-43R-5"	"0.0"	"47.0"	"226.440"	"226.675"	"226.910"	"226.25"	"226.476"	"226.701"	""	"1"	""	"Harzburgite with trace clinopyroxene and spinel. Contains patches and veins of reduced orthopyroxene proportions."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Several types of veins cut through the serpentinized peridotite including mesh, serpentine-magnetite veins (likely resulted to the mesh formation), fibrous chrysotile, and late massive and vuggy clay veins. The latter possibly overprint former magmatic veins. Serpentine-magnetite veins are crosscut by chrysotile and clay veins."	"Protogranular serpentinized harzburgite with weakly foliated horizontal mesh. Little white veins both horizontal and 60° dip.   "	
"399"	"U1601"	"C"	"44"	"R"	"1"	""	"399-U1601C-44R-1"	"0.0"	"111.0"	"226.700"	"227.255"	"227.810"	"226.7"	"227.192"	"227.685"	""	"1, 2, 3"	""	"Harzburgite with trace spinel. Thin veins of secondary material below 81 cm"	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Several types of veins occur in this section, including serpentine-magnetite, chrysotile, and late clay veins."	"Protogranular serpentinized harzburgite with weakly to modertely foliated horizontal mesh. Little white veins both horizontal and 60° dip.   "	
"399"	"U1601"	"C"	"44"	"R"	"2"	""	"399-U1601C-44R-2"	"0.0"	"149.0"	"227.810"	"228.555"	"229.300"	"227.685"	"228.346"	"229.008"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with trace spinel. Thin veins of secondary material traverse much of the length of the section. "	"Highly serpentinized harzburgite. Several types of veins containing serpentine-magnetite, chrysotile, and late clay veins occur in this section."	"Protogranular to weakly foliated porphyroclastic (horizontal mantle fabric serpentinized harzburgite, with moderate foliated to unfoliated (horizontal) mesh. Steeply dipping thick white veins, and subhorizontal little white veins. "	
"399"	"U1601"	"C"	"44"	"R"	"3"	""	"399-U1601C-44R-3"	"0.0"	"150.0"	"229.300"	"230.050"	"230.800"	"229.008"	"229.674"	"230.34"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Orthopyroxene-bearing dunite grading down to harzburgite, both with trace spinel."	"Highly serpentinized harzburgite. Several types of veins containing mesh, chrysotile, prehnite, and late clay veins. Prehnite and clay veins possibly overprint former magmatic veins."	"Protogranular serpentinized harzburgite with strongly foliated to unfoliated mesh. Opx dunite interval with strong, subhorizontal mesh. Little white veins parallel mesh and mantle fabric. Steep thick white veins. "	
"399"	"U1601"	"C"	"44"	"R"	"4"	""	"399-U1601C-44R-4"	"0.0"	"142.0"	"230.800"	"231.510"	"232.220"	"230.34"	"230.97"	"231.6"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace spinel and some interstitial clinopyroxene."	"Highly serpentinized harzburgite. Serpentine-magnetite veins are cut by chrysotile veins."	"Protogranular serpentinized harzburgite with unfoliated mesh; cut by moderate- to steeply dipping  white veins, and subhorizontal little white veins."	
"399"	"U1601"	"C"	"45"	"R"	"1"	""	"399-U1601C-45R-1"	"0.0"	"140.0"	"231.600"	"232.300"	"233.000"	"231.6"	"232.213"	"232.826"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace clinopyroxene and spinel. Cut by an oxide gabbronorite from 37-42 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Serpentine-magnetite, chrysotile, and late clay veins are present in serpentinite. Chrysotile and clay veins commonly cut altered magmatic veins. The upper part of the section (26-36) contains rubble of harzburgite and magmatic veins."	"Protogranular to weakly foliated porphyroclastic (10° dipping mantle fabric) serpentinized harzburgite with weakly foliated regular mesh. Cut by subhorozontal little white veins."	
"399"	"U1601"	"C"	"45"	"R"	"2"	""	"399-U1601C-45R-2"	"0.0"	"136.0"	"233.000"	"233.680"	"234.360"	"232.826"	"233.422"	"234.017"	""	"1, 2, 3, 4"	""	"Harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite. Serpentine-magnetite veins of variable thickness and chrysotile veins cut the rock."	"Protogranular to weakly foliated porphyroclastic (horizontal mantle fabric) serpentinized harzburgite with unfoliated to weakly foliated mesh.  "	
"399"	"U1601"	"C"	"45"	"R"	"3"	""	"399-U1601C-45R-3"	"0.0"	"129.0"	"234.360"	"235.005"	"235.650"	"234.017"	"234.582"	"235.147"	""	"1, 2, 3"	""	"Harzburgite with trace clinopyroxene and spinel. Has an interval of orthopyroxene-bearing dunite from 105-111cm."	"Highly serpentinized harzburgite and minor Opx-bearing dunite. Serpentine-magnetite, chrysotile, and picrolite cut the rock. The abundance of chrysotile veins decreases in dunite intervals."	"Protogranular to weakly foliated (horizontal) serpentinized harzburgite with unfoliated to weakly foliated mesh. Dunite intervals dip 45 °.  Sub-horizontal little white veins."	
"399"	"U1601"	"C"	"45"	"R"	"4"	""	"399-U1601C-45R-4"	"0.0"	"143.0"	"235.650"	"236.365"	"237.080"	"235.147"	"235.774"	"236.4"	""	"1, 2, 3, 4"	""	"Harzburgite with 1% clinopyroxene and trace spinel. A patchy medium-grain gabbro vein cuts the core at c. 4.5 cm."	"Highly serpentinized harzburgite cut by an hydrothermally altered magmatic vein. Serpentine-magnetite veins of variable thickness and chrysotile-picrolite veins cut through the serpentinite."	"Protogranular to weakly foliated porphyroclastic (horizontal) serpentinized harzburgite with unfoliated to weakly foliated mesh. Cut by one white green vein with moderate dip."	
"399"	"U1601"	"C"	"46"	"R"	"1"	""	"399-U1601C-46R-1"	"0.0"	"150.0"	"236.400"	"237.150"	"237.900"	"236.4"	"237.15"	"237.9"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite trace clinopyroxene and spinel. The harzburgite is cut by a 5 mm wide gabbro vein at c. 50 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. Serpentine-magnetite veins and chrysotile-picrolite veins cut the harzburgite. Chrysotile-picrolite veins cut the altered magmatic vein."	"Protogranular serpentinized harzburgite with patchy unfoliated mesh. Cut by a steeply dipping magmatic vein moderate to steeply dipping white and green veins."	
"399"	"U1601"	"C"	"46"	"R"	"2"	""	"399-U1601C-46R-2"	"0.0"	"135.0"	"237.900"	"238.575"	"239.250"	"237.9"	"238.575"	"239.25"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace clinopyroxene and spinel. The harzburgite is cut by a highly altered gabbro vein at c. 8 cm. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. Serpentine-magnetite, chrysotile, composite chrysotile-picrolite veins, and clay veins cut the harzburgite. Chrysotile, composite chrysotile-picrolite veins, and clay veins cut the altered magmatic vein."	"Protogranular serpentinized harzburgite with patchy regular mesh. Cut by moderately dipping green and white veins."	
"399"	"U1601"	"C"	"47"	"R"	"1"	""	"399-U1601C-47R-1"	"0.0"	"125.0"	"241.300"	"241.925"	"242.550"	"241.3"	"241.858"	"242.416"	""	"1, 2, 3, 4, 5"	""	"Harzburgite and dunite with intervening gradational proportions of orthopyroxene. Trace clinopyroxene and spinel in harzburgite. The dunite has trace spinel."	"Highly serpentinized harzburgite and dunite. Serpentine-magnetite of variable thickness and chrysotile-picrolite veins cut through the rock. The abundance of chrysotile veins decreases in the dunite interval."	"Protogranular to porphyroclastic (0-45° dipping mantle fabric) serpentinized harzburgite with intervals of gently dipping dunite. Unfoliated serpentine mesh. Little white veins with multiple overlapping orientations.  "	
"399"	"U1601"	"C"	"47"	"R"	"2"	""	"399-U1601C-47R-2"	"0.0"	"150.0"	"242.550"	"243.300"	"244.050"	"242.416"	"243.086"	"243.756"	""	"1"	""	"Harzburgite with dunite between 22.5 and 26 cm. Trace clinopyroxene and spinel in harzburgite. The dunite jhas 1% spinel."	"Highly serpentinized harzburgite and dunite. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the peridotites. The number of chrysotile veins decreases in dunite intervals."	"Protogranular to porphyroclastic (15-30° dipping mantle fabric) serpentinized harzburgite with intervals of dunite hosting spinel trails. And regular patchy mesh. Little white veins subparallel to mantle fabric.  One piece end fault with steep slickenfibers. "	
"399"	"U1601"	"C"	"47"	"R"	"3"	""	"399-U1601C-47R-3"	"0.0"	"128.0"	"244.050"	"244.690"	"245.330"	"243.756"	"244.327"	"244.899"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with trace proportions of clinopyroxene and spinel."	"Highly serpentinized harzburgite. Serpentine-magnetite veins of variable thickness, chrysotile, and massive green picrolite veins cut through the serpentinite."	"Protogranular to porphyroclastic (15-30° dipping mantle fabric) serpentinized harzburgite  Unfoliated to moderately foliated mesh parallel to mantle fabric. Little white veins subparallel to mantle fabric. 2nd generationwhite veins cross cut 1st generation. Green white, and magnetite veins are moderately dipping."	
"399"	"U1601"	"C"	"47"	"R"	"4"	""	"399-U1601C-47R-4"	"0.0"	"134.5"	"245.330"	"246.002"	"246.675"	"244.899"	"245.498"	"246.096"	""	"1, 2, 3, 4"	""	"Harzburgite with trace proportions of clinopyroxene and spinel."	"Highly serpentinized harzburgite. Serpentine-magnetite veins of variable thickness, chrysotile, and massive green picrolite veins cut through the serpentinite."	"Protogranular serpentinized harzburgite with localized patchy regular mesh. Little white veins subhorizontal to 30° dip.  "	
"399"	"U1601"	"C"	"48"	"R"	"1"	""	"399-U1601C-48R-1"	"0.0"	"93.0"	"246.100"	"246.565"	"247.030"	"246.1"	"246.565"	"247.03"	""	"1"	""	"Harzburgite with trace spinel. Has a dunite band at c. 30 cm with unusually sharp contacts. "	"Highly serpentinized harzburgite with minor dunite. Serpentine-magnetite veins of variable thickness, chrysotile, and massive green picrolite veins cut through the serpentinized harzburgite. The chrysotile and picrolite veins are absent in serpentinized dunite (26-31 cm)."	"Protogranular to porphyroclastic (horizontal dipping mantle fabric) serpentinized harzburgite with dunite interval (35° contact). No mesh except in dunite where  horizontal.High density of horizontal little white veins."	
"399"	"U1601"	"C"	"48"	"R"	"2"	""	"399-U1601C-48R-2"	"0.0"	"119.0"	"247.030"	"247.625"	"248.220"	"247.03"	"247.625"	"248.22"	""	"1"	""	"Harzburgite with dunite horizons at c. 20 and 100 cm. The lower dunite horizon has a central olivine gabbronorite vein. The peridotites all have trace chromite."	"Highly serpentinized harzburgite with minor dunite (18-22 and 96-101 cm); the latter is cut by one hydrothermally altered magmatic vein (98-99 cm). Serpentine-magnetite veins of variable thickness, chrysotile, and massive green to white picrolite veins cut through the serpentinite. The proportion of the chrysotile veins decreases in the dunite intervals"	"Protogranular to porphyroclastic (horizontal mantle fabric) serpentinized harzburgite with dunite interval (20-40° contacts). No mesh to weakly foliated mesh. High density of little white veins, with horizontal to 20° dip."	
"399"	"U1601"	"C"	"48"	"R"	"3"	""	"399-U1601C-48R-3"	"0.0"	"138.0"	"248.220"	"248.910"	"249.600"	"248.22"	"248.91"	"249.6"	""	"1, 2, 3"	""	"Harzburgite with trace spinel, two textures of orthopyroxene are evident."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. This section appears to be fresher than the previous sections. Several types of veins including serpentine-magnetite veins, chrysotile, and massive green-to-white picrolite veins cut through the harzburgite."	"Porphyroclastic serpentinized harzburgite (0-20°) with no to localized patchy regular mesh. Little white veins subparallel mantle fabric. Density of little white veins is high. Moderately to steeply dipping green and white veins, one piece end fault with steep plunge."	
"399"	"U1601"	"C"	"48"	"R"	"4"	""	"399-U1601C-48R-4"	"0.0"	"106.0"	"249.600"	"250.130"	"250.660"	"249.6"	"250.13"	"250.66"	""	"1, 2, 3, 4"	""	"Harzburgite with trace spinel, relatively coarse grained from 80 cm on."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein (0-14 cm). Several types of veins including serpentine-magnetite, chrysotile, and massive green-to-white picrolite veins cut through the harzburgite and the magmatic vein."	"Porphyroclastic weakly foliated (10° dipping mantle fabric) serpentinized harzburgite with localized patchy regular mesh. Little white veins dip 20°-35°.   One steep altered magmatic vein, and  green veins."	
"399"	"U1601"	"C"	"49"	"R"	"1"	""	"399-U1601C-49R-1"	"0.0"	"75.5"	"251.000"	"251.377"	"251.755"	"251"	"251.377"	"251.755"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace spinel and an unusually high clinopyroxene abundance from 80 cm onward (perhaps as high as 2 wt% ). Cut by 2 minor gabbro veins."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins (45-54 and 65-66 cm). Several types of veins including serpentine-magnetite veins, chrysotile, and massive green to white picrolite veins cut the serpentinite. Picrolite veins cut the magmatic veins."	"Protogranular serpentinized harzburgite with localized regular mesh. Little white veins dip 20°. Magmatic, green, white veins with moderate dips."	
"399"	"U1601"	"C"	"49"	"R"	"2"	""	"399-U1601C-49R-2"	"0.0"	"118.0"	"251.755"	"252.345"	"252.935"	"251.755"	"252.345"	"252.935"	""	"1"	""	"Harzburgite with trace clinopyroxene and spinel"	"Highly serpentinized harzburgite. Extent of serpentinization is variable. Several types of veins including serpentine-magnetite veins, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Porphyroclastic serpentinized harzburgite (with subhorizontal mantle fabric) and no mesh. Little white veins subparallel to mantle fabric. Gently to moderately dipping green veins."	
"399"	"U1601"	"C"	"49"	"R"	"3"	""	"399-U1601C-49R-3"	"0.0"	"112.0"	"252.935"	"253.495"	"254.055"	"252.935"	"253.495"	"254.055"	""	"1, 2"	""	"Harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite with lower amounts of orthopyroxene at the top of the section (3-13 cm). The extent of serpentinization is variable. Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. The proportion of chrysotile veins strongly decreases in the Opx-poor harzburgite interval."	"Protogranular to weakly porphyroclastic (10° dippng mantle fabric) serpentinized harzburgite with no mesh. Little white veins dip subparallel mantle fab. Reverse piece-end fault."	
"399"	"U1601"	"C"	"49"	"R"	"4"	""	"399-U1601C-49R-4"	"0.0"	"118.0"	"254.055"	"254.645"	"255.235"	"254.055"	"254.645"	"255.235"	""	"1, 2, 3"	""	"Harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite cut by three hydrothermally altered magmatic veins (50-51, 55-56, and 66-67 cm). Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. Picrolite also locally crosscut the last magmatic vein."	"Protogranular serpentinized harzburgite with no regular mesh. Crosscutting magmatic vein (moderate) and green picrolite veins (shallow). Little white veins dip 10°. "	
"399"	"U1601"	"C"	"49"	"R"	"5"	""	"399-U1601C-49R-5"	"0.0"	"55.5"	"255.235"	"255.512"	"255.790"	"255.235"	"255.512"	"255.79"	""	"1"	""	"Harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins (7 to 18 cm). Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Protogranular serpentinized harzburgite with no regular mesh. Crosscutting green picrolite veins (shallow), and piece end fault."	
"399"	"U1601"	"C"	"50"	"R"	"1"	""	"399-U1601C-50R-1"	"0.0"	"146.0"	"255.800"	"256.530"	"257.260"	"255.8"	"256.53"	"257.26"	""	"1, 2, 3, 4"	""	"Harzburgite, granular and interstitial opx and trace spinel. The interval from 6 - 11 cm is a lherzolitic band which was likely due to a magmatic infusion."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Minor serpentinized Ol-clinopyroxenite at the top of the section (7-11 cm). Several types of veins including serpentine, chrysotile, and massive green picrolite veins cut through the harzburgite and the clinopyroxenite. Picrolite veins cut the magmatic vein."	"Protogranular serpentinized harzburgite with no mesh. Pyroxenite interval dips 35°.  Crosscutting green picrolite veins shallow to vertical, cut by little white veins dip 10-20°. "	
"399"	"U1601"	"C"	"50"	"R"	"2"	""	"399-U1601C-50R-2"	"0.0"	"127.0"	"257.260"	"257.895"	"258.530"	"257.26"	"257.895"	"258.53"	""	"1, 2, 3, 4"	""	"The upper 41 cm is an olivine-bearing dunite cut by a gabbronorite vein at 24-26 cm, which has orthopyroxene lining its contacts. Beneath 41 cm is a harzburgite with c. 15% orthopyroxene and bearing  thin websterite veins at 63 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins (main one is 22-24 cm). Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Protogranular serpentinized harzburgite with patchy regular mesh. Magmatic veins dip 60¿, cut by green picrolite and thin white veins."	
"399"	"U1601"	"C"	"50"	"R"	"3"	""	"399-U1601C-50R-3"	"0.0"	"88.0"	"258.530"	"258.970"	"259.410"	"258.53"	"258.97"	"259.41"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with trace cpx and spinel. The orthopyroxene has both granular and interstitial textures."	"Highly serpentinized harzburgite with variable Opx abundance cut by hydrothermally altered magmatic veins. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. Chrysotile vein cut the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh. White veins with 0 to 45° dip, with shallow dips cutting steeper veins. Moderately- to steeply dipping green and white veins. "	
"399"	"U1601"	"C"	"50"	"R"	"4"	""	"399-U1601C-50R-4"	"0.0"	"93.0"	"259.410"	"259.875"	"260.340"	"259.41"	"259.875"	"260.34"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace cpx and spinel. The orthopyroxene has both granular and interstitial textures."	"Highly serpentinized harzburgite with variable Opx abundance cut by hydrothermally altered magmatic veins. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. Chrysotile/picrolite vein cut the magmatic veins. The picrolite veins also overprint the serpentine-magnetite veins."	"Protogranular serpentinized harzburgite with no mesh.  Moderately dipping  little white veins and green veins with 25°dip."	
"399"	"U1601"	"C"	"51"	"R"	"1"	""	"399-U1601C-51R-1"	"0.0"	"140.0"	"260.700"	"261.400"	"262.100"	"260.7"	"261.4"	"262.1"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with granular and interstitial orthopyroxene, as well as trace clinopyroxene. "	"Highly serpentinized harzburgite with variable Opx abundance cut by hydrothermally altered magmatic veins. Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite and the magmatic veins. The picrolite veins also overprint the serpentine-magnetite veins."	"Protogranular serpentinized harzburgite with patchy regular mesh. Cut by moderate dip (55-65° dip), 10-60° dipping green-white veins and  sub-horizontal little white veins."	
"399"	"U1601"	"C"	"51"	"R"	"2"	""	"399-U1601C-51R-2"	"0.0"	"145.5"	"262.100"	"262.827"	"263.555"	"262.1"	"262.827"	"263.555"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with trace clinopyroxene. Contains rare veins filled with secondary minerals that may have once been magmatic."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The bottom of the section contains rubble of magmatic veins and harzburgite. Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite and the magmatic veins. The picrolite veins also overprint the serpentine-magnetite veins."	"Protogranular serpentinized harzburgite with no mesh, cut by gently dipping green veins and subhorizontallittle white veins."	
"399"	"U1601"	"C"	"51"	"R"	"3"	""	"399-U1601C-51R-3"	"0.0"	"106.0"	"263.555"	"264.085"	"264.615"	"263.555"	"264.085"	"264.615"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with trace to percent-scale clinopyroxene. Clinopyroxene proportions generally increase down section, with a maximum of c. 2 wt.% at interval 81 to 105 cm. A 3mm wide highly altered magmatic vein may be found at 66-75cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite and the magmatic veins. The picrolite veins also locally overprint the serpentine-magnetite veins."	"Protogranular serpentinized harzburgite with weakly foliated subhorizontal mesh. Cut by moderate dip magmatic veins, green veins, and subhorizontal little white veins. "	
"399"	"U1601"	"C"	"51"	"R"	"4"	""	"399-U1601C-51R-4"	"0.0"	"72.0"	"264.615"	"264.975"	"265.335"	"264.615"	"264.975"	"265.335"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Garden variety harzburgite."	"Highly serpentinized harzburgite. Serpentinite rubble contains altered magmatic veinlets. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Protogranular serpentinized harzburgite with no mesh. Cut by subhorizontal little white veins."	
"399"	"U1601"	"C"	"52"	"R"	"1"	""	"399-U1601C-52R-1"	"0.0"	"129.0"	"265.500"	"266.145"	"266.790"	"265.5"	"266.063"	"266.625"	""	"1, 1, 2, 2, 3, 3, 4, 4, 5, 5, 6, 7, 8"	""	"Harzburgite with granular and interstitial orthopyroxene. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite and the magmatic veins."	"Protogranular serpentinized harzburgite with patchy regular mesh. Magmatic veins (moderately dipping) cut by green and white veins (moderately dipping)."	
"399"	"U1601"	"C"	"52"	"R"	"2"	""	"399-U1601C-52R-2"	"0.0"	"62.0"	"266.790"	"267.100"	"267.410"	"266.625"	"266.894"	"267.164"	""	"1, 1"	""	"Harzburgite with granular and interstitial orthopyroxene. "	"Highly serpentinized harzburgite. Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Protogranular serpentinized harzburgite with patchy regular mesh. Little white veins with variable dip (shallow to moderate)."	
"399"	"U1601"	"C"	"52"	"R"	"3"	""	"399-U1601C-52R-3"	"0.0"	"135.5"	"267.410"	"268.087"	"268.765"	"267.165"	"267.755"	"268.344"	""	"1, 1, 2, 2, 3, 3, 4, 4, 5, 5, 6, 6, 7"	""	"Harzburgite with granular and interstitial orthopyroxene. Gabbronorite vein near the base with orthopyroxene concentrated near the reactive contact with harzburgite."	"Highly serpentinized harzburgite crosscut by thick magmatic vein at the bottom of the section (97-135 cm). Serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. Carbonate-zeolite veins cut through the hydrothermal magmatic vein and progressively extend to picrolite veins in the serpentinized harzburgite."	"Protogranular serpentinized harzburgite with patchy regular mesh. 4 cm thick magmatic vein is cut by later horizontal magmatic vein. White veins (moderately dipping)."	
"399"	"U1601"	"C"	"52"	"R"	"4"	""	"399-U1601C-52R-4"	"0.0"	"144.5"	"268.765"	"269.488"	"270.210"	"268.347"	"268.997"	"269.647"	""	"1, 1, 2, 2, 3, 3, 4, 5, 6, 7"	""	"Harzburgite with granular and interstitial orthopyroxene. Gabbronorite vein near the base with orthopyroxene concentrated near the reactive contact with harzburgite."	"Highly serpentinized harzburgite crosscut by thick magmatic vein at the top of the section (0-4 cm). Relicts olivine in some parts of the section. Several types of veins including mesh, serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite. Carbonate-zeolite veins cut through the hydrothermal magmatic vein. Carbonate-zeolite veins turn into picrolite veins in the serpentinized harzburgite."	"Protogranular serpentinized harzburgite with patchy regular mesh. Steep magmatic vein cut by green veins; little white veins subhorizontal."	
"399"	"U1601"	"C"	"52"	"R"	"5"	""	"399-U1601C-52R-5"	"0.0"	"91.0"	"270.210"	"270.665"	"271.120"	"269.607"	"270.003"	"270.4"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with granular and interstitial orthopyroxene. "	"Highly serpentinized harzburgite possibly crosscut by diffuse hydrothermally altered magmatic vein (55 cm). Relicts of olivine occur in some parts of the section. Several types of veins including serpentine-magnetite, chrysotile, and massive green picrolite veins cut through the harzburgite."	"Protogranular serpentinized harzburgite with patchy regular mesh. Several moderately dipping magmatic veins cut by little white veins subhorizontal."	
"399"	"U1601"	"C"	"53"	"R"	"1"	""	"399-U1601C-53R-1"	"0.0"	"110.5"	"270.400"	"270.952"	"271.505"	"270.4"	"270.952"	"271.505"	""	"1, 2"	""	"The commonplace harzburgite"	"Serpentinized harzburgite with abundant chrysotile veins. Sparse spinel appears unaltered. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. Sub-parallel chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Porphyroclastic (subhorizontal) serpentinized harzburgite with regular mesh. Little white veins subparallel to mantle fabric."	
"399"	"U1601"	"C"	"53"	"R"	"2"	""	"399-U1601C-53R-2"	"0.0"	"106.0"	"271.505"	"272.035"	"272.565"	"271.505"	"272.035"	"272.565"	""	"1"	""	"The commonplace harzburgite with thin irregular veins composed of secondary minerals near the base that may have originally been magmatic."	"Serpentinized harzburgite cut by hydrothermally altered magmatic veinlet and containing abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. Sub-parallel chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Porphyroclastic (subhorizontal) serpentinized harzburgite with regular mesh. Little white veins subparallel to mantle fabric."	
"399"	"U1601"	"C"	"53"	"R"	"3"	""	"399-U1601C-53R-3"	"0.0"	"125.0"	"272.565"	"273.190"	"273.815"	"272.565"	"273.19"	"273.815"	""	"1"	""	"Orthopyroxene-bearing  dunite for the top 10 cm. Harzburgite is below interspersed with a variety of gabbroic veins, including a steely dipping medium grained gabbro centered at c. 87 cm, a coarse grained gabbronorite centered at c. 104 cm, and a leucocratic diorite vein cutting the harzburgite and gabbro at c. 114 cm."	"Serpentinized harzburgite with a 3-5 cm wide hydrothermally altered magmatic vein. Olivine and orthopyroxene are quite fresh close to the magmatic vein compared to the matrix farther away from the vein. The magmatic vein is cut by a 1-cm wide composite carbonate vein. In the remainder of the harzburgite, the extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. Sub-parallel chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite. The magmatic vein is crosscut by carbonate-zeolite veins that grade to picrolite, while propagating into the serpentinized harzburgite further away from the magmatic vein."	"Porphyroclastic (10° mantle fabric dip) serpentinized harzburgite with weakly foliated incipient to patchy regular mesh. Little white veins subparallel to mantle fabric. Network of cross cutting magmatic veins, 3 generations, all cut by serpentine veins."	
"399"	"U1601"	"C"	"53"	"R"	"4"	""	"399-U1601C-53R-4"	"0.0"	"73.0"	"273.815"	"274.180"	"274.545"	"273.815"	"274.18"	"274.545"	""	"1, 2"	""	"Harzburgite with the grain size of orthopyroxene increasing down section."	"Serpentinized harzburgite with abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine is present in Opx-richer layers. Sub-parallel chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Porphyroclastic (15° dip) serpentinized harzburgite with weakly foliated parallel mesh. Little white veins are subparallel to mantle fabric. One vertical white vein."	
"399"	"U1601"	"C"	"54"	"R"	"1"	""	"399-U1601C-54R-1"	"0.0"	"121.5"	"275.200"	"275.808"	"276.415"	"275.2"	"275.692"	"276.184"	""	"1"	""	"Harzburgite with granular and interstitial orthopyroxene. An orthopyroxene-bearing dunite at 34-42 cm has only the rounded, granular orthopyroxene."	"Serpentinized harzburgite with abundant chrysotile veins. Sparse spinel appears unaltered. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine is present in Opx-richer layers. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Protogranular to porphyroclastic (10° dip) serpentinized harzburgite with moderate (10° dip) to patchy regular mesh. Little white veins of variable orientation."	
"399"	"U1601"	"C"	"54"	"R"	"2"	""	"399-U1601C-54R-2"	"0.0"	"82.5"	"276.415"	"276.827"	"277.240"	"276.184"	"276.518"	"276.852"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with rounded and interstitial orthopyroxene textures. Contains 10 cm zones with lower orthopyroxene proportions and only the rounded and larger orthopyroxene grains. These zones are akin to the opx-bearing dunite in section 1."	"Serpentinized harzburgite with abundant chrysotile veins. Sparse spinel appears unaltered. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Protogranular serpentinized harzburgite with weakly foliated mesh dipping 15°. Cut by sreen and white veins with moderate to steep dips. Little white veins with dip of 30°."	
"399"	"U1601"	"C"	"54"	"R"	"3"	""	"399-U1601C-54R-3"	"0.0"	"143.0"	"277.240"	"277.955"	"278.670"	"276.852"	"277.431"	"278.01"	""	"1, 2, 3, 4"	""	"Harzburgite with rounded and interstitial orthopyroxene textures. The top 8 cm is a dunite with granular orthopyroxene"	"Serpentinized harzburgite with abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite. Small hydrothermally altered magmatic patch."	"Porphyroclastic (15° dipping mantle fabric) serpentinized harzburgite with patchy regular mesh. Little white veins and green veins subparallel to mantle fabric."	
"399"	"U1601"	"C"	"54"	"R"	"4"	""	"399-U1601C-54R-4"	"0.0"	"150.0"	"278.670"	"279.420"	"280.170"	"278.01"	"278.618"	"279.225"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with rounded and interstitial orthopyroxene textures. Contains 10 cm zones with lower orthopyroxene proportions and only the rounded and larger orthopyroxene grains. These zones are akin to the opx-bearing dunite in section 1."	"Serpentinized harzburgite with abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine occurs in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite. One larger (5 mm wide) subhorizontal picrolite vein cuts through the core in piece 5."	"Protogranular to porphyroclastic(shallow dip) serpentinized harzburgite with patchy regular to moderately foliated mesh. Green veins, piece end fault, cut by white veins."	
"399"	"U1601"	"C"	"54"	"R"	"5"	""	"399-U1601C-54R-5"	"0.0"	"88.0"	"280.170"	"280.610"	"281.050"	"279.225"	"279.582"	"279.938"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with two textures - rounded and interstitial. "	"Serpentinized harzburgite with abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Porphyroclastic (5° dipping mantle fabric) serpentinized harzburgite with moderately foliated parallel mesh cut by one white vein, shallowly dipping."	
"399"	"U1601"	"C"	"55"	"R"	"1"	""	"399-U1601C-55R-1"	"0.0"	"94.0"	"280.100"	"280.570"	"281.040"	"280.1"	"280.57"	"281.04"	""	"1, 2, 3"	""	"Harzburgite with cm-scale dunite channels. Trace clinopyroxene and spinel are present."	"Serpentinized harzburgite with abundant chrysotile veins. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Protogranular serpentinized harzburgite with regular mesh, cut by shallow little white veins cut by moderately dipping green veins."	
"399"	"U1601"	"C"	"55"	"R"	"2"	""	"399-U1601C-55R-2"	"0.0"	"94.0"	"281.040"	"281.510"	"281.980"	"281.04"	"281.51"	"281.98"	""	"1"	""	"Harzburgite with cm-scale dunite channels. Trace clinopyroxene and spinel are present."	"Serpentinized harzburgite with abundant chrysotile veins. One thin hydrothermally altered magmatic vein (1mm). The extent of serpentinization is variable on a mm- to cm-scale. There is more relict olivine in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Protogranular serpentinized harzburgite with regular  mesh, cut by white veins with variable dips of 35-50°, and moderately dipping green veins."	
"399"	"U1601"	"C"	"55"	"R"	"3"	""	"399-U1601C-55R-3"	"0.0"	"114.0"	"281.980"	"282.550"	"283.120"	"281.98"	"282.55"	"283.12"	""	"1, 2, 3"	""	"Harzburgite with cm-scale dunite channels. Trace clinopyroxene and spinel are present."	"Serpentinized harzburgite with abundant chrysotile veins. Thin hydrothermally altered magmatic veins (2mm) with halo. The extent of serpentinization is variable on a mm- to cm-scale. More relict olivine in Opx-richer layers. The amount of talc in bastite appears to be variable. In most cases, bastite consists of serpentine with little or no talc. Chrysotile veins appear to be more abundant in mesh or at the boundary of mesh and bastite."	"Porphyroclastic (subhorizontal mantle fabric) serpentinized harzburgite with regular mesh. Altered magmatic vein with moderate dip and white and green veins with shallow dip. Late, little white veins dip 0-20°."	
"399"	"U1601"	"C"	"56"	"R"	"1"	""	"399-U1601C-56R-1"	"0.0"	"126.0"	"284.900"	"285.530"	"286.160"	"284.9"	"285.448"	"285.996"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with two textures - rounded and interstitial. Contains a 1 cm wide pyroxenite (likely websterite) vein centered at c. 77 cm with sharp, irregular contacts against the harzburgite."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. The latter is made of chlorite, prehnite, amphibole, and one pink mineral. Possible rodingite. Some areas show a variable extent of serpentinization with relict olivine. Bastite is composed of serpentine and in some cases serpentine and talc. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular to weakly porphyroclastic (horizontal) serpentinized harzburgite with patchy regular mesh. White and green veins with shallow dips.Little white veins have variable dips of 15-30°."	
"399"	"U1601"	"C"	"56"	"R"	"2"	""	"399-U1601C-56R-2"	"0.0"	"134.5"	"286.160"	"286.832"	"287.505"	"286"	"286.585"	"287.17"	""	"1, 2"	""	"Harzburgite with two textures - rounded and interstitial. Contains a 2 mm wide gabbro vein centered at c. 129 cm with sharp, irregular contacts against the harzburgite."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. The latter is made of chlorite, prehnite, amphibole, and one pink mineral. Possible rodingite. Some areas contain fresh olivine (variable extent of serpentinization). The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter also cut through the magmatic veins."	"Weakly porphyroclastic (subhorizontal mantle fabric) serpentinized harzburgite with patchy regular mesh. Several magmatic veins with steep dips, cut by Llittle white veins variable dips."	
"399"	"U1601"	"C"	"56"	"R"	"3"	""	"399-U1601C-56R-3"	"0.0"	"137.0"	"287.505"	"288.190"	"288.875"	"287.173"	"287.771"	"288.369"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with two textures - rounded and interstitial. Contains a 2 mm wide gabbro vein centered at c. 129 cm with sharp, irregular contacts against the harzburgite. This is the same vein as in section 56R-2."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. The latter is made of chlorite, prehnite, amphibole, and one pink mineral. Possible rodingite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine and in some cases serpentine and talc. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter also cut through the magmatic veins."	"Porphyroclastic (0-10° dipping mantle fabric) serpentinized harzburgite with weakly foliated mesh. Steep magmatic vein and shallow green veins, cut by little white veins that dip parallel to mantle foliation."	
"399"	"U1601"	"C"	"56"	"R"	"4"	""	"399-U1601C-56R-4"	"0.0"	"97.5"	"288.875"	"289.363"	"289.850"	"288.369"	"288.793"	"289.217"	""	"1, 2, 3, 4"	""	"Harzburgite with two textures - rounded and interstitial. Contains two 2 mm wide gabbro veins towards the center of the section with sharp, irregular contacts against the harzburgite. These veins are of the same type as in the preceding two sections."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The altered magmatic veins are composed of chlorite, prehnite, amphibole, and one pink mineral. Possible rodingite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine and in some cases serpentine and talc. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter also cut through the magmatic veins."	"Protogranular to weakly porphyroclastic (15-20° dipping fabric) serpentinized harzburgite with regular mesh.   One steeply dipping magmatic vein, cut by  lLittle white veins parallel to mantle fabric."	
"399"	"U1601"	"C"	"56"	"R"	"CC"	""	"399-U1601C-56R-CC"	"0.0"	"31.0"	"289.800"	"289.955"	"290.110"	"289.508"	"289.654"	"289.8"	""	""	""	"Harzburgite with both granular and interstitial opx."	"Highly serpentinized harzburgite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine and in some cases serpentine and talc. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh and a network of fibrous to massive chrysotile veins."	"Porphyroclastic serpentinized harzburgite (10° dip) with moderately foliated mesh. Little white veins are parallel to mantle fabric."	
"399"	"U1601"	"C"	"57"	"R"	"1"	""	"399-U1601C-57R-1"	"0.0"	"121.5"	"289.800"	"290.408"	"291.015"	"289.8"	"290.365"	"290.93"	""	"1"	""	"Harzburgite with mostly granular and some interstitial orthopyroxene. Orthopyroxene proportions vary from c. 10-15 %."	"Highly serpentinized harzburgite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh and a network of fibrous to massive chrysotile veins."	"Porphyroclastic serpentinized harzburgite (25° dip) with regular mesh. Little white veins are parallel to mantle fabric."	
"399"	"U1601"	"C"	"57"	"R"	"2"	""	"399-U1601C-57R-2"	"0.0"	"67.0"	"291.015"	"291.350"	"291.685"	"290.925"	"291.236"	"291.548"	""	"1, 2, 3, 4"	""	"Harzburgite with granular and rarer interstitial orthopyroxene. Piece 1 has trains of coarse orthopyroxene surrounded by vein-like olivine-rich areas on the cm scale."	"Highly serpentinized harzburgite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with regular mesh. Several white and green veins with shallow to moderately dip, one piece end fault."	
"399"	"U1601"	"C"	"57"	"R"	"3"	""	"399-U1601C-57R-3"	"0.0"	"125.0"	"291.685"	"292.310"	"292.935"	"291.545"	"292.123"	"292.702"	""	"1"	""	"Harzburgite with granular and some interstitial othopyroxene above an orthopyroxene-bearing dunite that borders a zoned 10 cm wide gabbroic intrusion. The core of the intrusion is coarse-grained gabbronorite. The margins are medium-grained olivine gabbro; interpreted as reaction boundaries. Harzburgite with increasing orthopyroxene concentration away from the gabbro contact is below 199 cm. "	"Highly serpentinized harzburgite cut by a hydrothermally altered gabbro vein at the bottom of the section. The altered magmatic vein is made of chlorite, secondary plagioclase after plagioclase, and amphibole after clinopyroxene. Some areas contain fresh olivine (variable extent of serpentinization). At the top of the section, bastite is  green and completely altered to serpentine, while down section bastite is grey and locally contains a light core that is preserved orthopyroxene. Bastite is composed of serpentine. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with no mesh. Thin gabbro interval with moderately dipping contact cut by white-gray veins.  "	
"399"	"U1601"	"C"	"57"	"R"	"4"	""	"399-U1601C-57R-4"	"0.0"	"139.0"	"292.935"	"293.630"	"294.325"	"292.702"	"293.346"	"293.989"	""	"1, 2, 3, 4"	""	"Harzburgite with granular and interstitial orthopyroxene. Between 90 and 95 cm is a dunite with rare orthopyroxene. Trails of chromium spinels cut the dunite at a high angle."	"Highly serpentinized harzburgite. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite to white serpentine veins."	"Porphyroclastic serpentinized harzburgite (25° dipping mantle fabric) with moderately foliated mesh (15° dip); dunite interval with shallow contact and weakly foliated mesh (15° dip).  One magmatic vein with moderate dip."	
"399"	"U1601"	"C"	"57"	"R"	"5"	""	"399-U1601C-57R-5"	"0.0"	"66.0"	"294.325"	"294.655"	"294.985"	"293.989"	"294.295"	"294.6"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with prominent granular orthopyroxene. A coarse grained olivine gabbro cuts the harzburgite at 50-66 cm. The reaction boundary between the gabbro and harzburgite is troctolitic."	"Highly serpentinized harzburgite cut by a hydrothermally altered gabbro vein at the bottom of the section. Gabbro is altered to amphibole (two types, brown and black) after clinopyroxene and chlorite, prehnite, and secondary plagioclase after plagioclase. It is cut by anastomosing prehnite-chlorite veins. Some areas contain fresh olivine (variable extent of serpentinization). Bastite is composed of serpentine. Spinel looks fresh. Long chrysotile fibers at piece ends. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and chrysotile-carbonate veins."	"Porphyroclastic serpentinized harzburgite (15° dip) with no mesh. Little white veins parallel mantle fabric. Gabbro interval with 35° dipping upper contact against serpentinized harzburgite."	
"399"	"U1601"	"C"	"58"	"R"	"1"	""	"399-U1601C-58R-1"	"0.0"	"121.0"	"294.600"	"295.205"	"295.810"	"294.6"	"295.199"	"295.798"	""	"1, 2, 3, 4, 5"	""	"The top bins have two gabbro pebbles that are likely accidental. The rest of the section is harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein. Some pebbles of gabbro at the top of the section. In the gabbro, plagioclase is altered to secondary plagioclase, chlorite and prehnite, and clinopyroxene is altered to amphibole. Some areas contain fresh olivine, variable extent of serpentinization. Bastite is composed of serpentine. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, thick serpentine-magnetite veins that cut the mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins. The latter cut through the hydrothermally altered magmatic vein."	"Gabbro rollers above protogranular serpentinized harzburgite, with regular mesh and little white veins (both 15° dip). Cut by several white and green veins with moderate dips."	
"399"	"U1601"	"C"	"58"	"R"	"2"	""	"399-U1601C-58R-2"	"0.0"	"130.0"	"295.810"	"296.460"	"297.110"	"295.798"	"296.442"	"297.085"	""	"1, 2, 3, 4"	""	"Harzburgite like that in the previous section. At 112-127, the harzburgite is strongly deformed, and it has less orthopyroxene. The base is highly deformed dunite."	"Highly serpentinized harzburgite and minor dunite. Bastite is composed of serpentine. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins."	"Porphyroclastic serpentinized harzburgite (15° dip) with no to regualr mesh. Little white veins parallel to mantle fabric. Dunite interval with moderate serpentine mesh (25° dip).  interval of protogranular mantle at 67-107cm have unusual fabric with trains of larger opx grains.  Cut by white and green veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"58"	"R"	"3"	""	"399-U1601C-58R-3"	"0.0"	"120.0"	"297.110"	"297.710"	"298.310"	"297.085"	"297.679"	"298.273"	""	"1, 2, 3, 4, 5, 6, 7"	""	"The top 33 cm is highly deformed, varying downward from orthopyroxene-bearing dunite to dunite. Below is coarse-grained seriate granular olivine-bearing gabbro with coarser grains at the center and finer grains at the margin."	"Hydrothermally altered coarse-grained gabbro and serpentinized dunite. The gabbro is made of amphibole after clinopyroxene, and chlorite, prehnite and secondary plagioclase after plagioclase. It is cut by chlorite and quartz-carbonate-sulfide veins. Fresh spinel is present in dunite. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh and a network of fibrous to massive chrysotile veins."	" Dunite, and with stretched lighter colored intervals, plus little white veins which are unusual for dunite. gabbro isotropic with grain size layering, shallow to moderately dipping.  Moderately dipping white and green veins.      "	
"399"	"U1601"	"C"	"58"	"R"	"4"	""	"399-U1601C-58R-4"	"0.0"	"124.0"	"298.310"	"298.930"	"299.550"	"298.273"	"298.887"	"299.5"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Highly deformed dunite above harzburgite with deformation decreasing down-section."	"Highly serpentinized dunite and harzburgite.The dunite is cut by a hydrothermally altered magmatic vein (end of a piece). Bastite is composed of serpentine. Spinel looks fresh in both dunite and harzburgite. Mesh in the harzburgite is yellowish green. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins."	"Dunite with strong mesh foliation (15° dip) and protogranular serpentinized harzburgite withno to regualr mesh.  Contact between dunite and harzburgite is dipping 20°. Cut by several white veins with shallow to steep dips."	
"399"	"U1601"	"C"	"59"	"R"	"1"	""	"399-U1601C-59R-1"	"0.0"	"150.0"	"299.500"	"300.250"	"301.000"	"299.5"	"300.25"	"301"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with increased orthopyroxene concentrations up-section. Trace spinel. Thin gabbronorite veins are scattered through the section."	"Highly serpentinized harzburgite cut by a thin hydrothermally altered magmatic vein. The latter is made of chlorite, amphibole, secondary plagioclase, and prehnite. Bastite is composed of serpentine and is locally black close to olive green veins (serpentine?). There, bastite has a pistachio-colored halo. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive dark-haloed green picrolite veins."	"Protogranular serpentinized harzburgite with moderately foliated (5° dip) to patchy regular mesh. Several magmatic veins with steep dips cut by green white veins.  Several green and white veins with moderate dips."	
"399"	"U1601"	"C"	"59"	"R"	"2"	""	"399-U1601C-59R-2"	"0.0"	"120.0"	"301.000"	"301.600"	"302.200"	"301"	"301.6"	"302.2"	""	"1"	""	"Harzburgite with trace spinel. Contains wispy magmatic veins of uncertain composition as a result of alteration."	"Highly serpentinized harzburgite with variable abundances of orthopyroxene cut by thin hydrothermally altered magmatic veins. The latter is made of chlorite, amphibole, secondary plagioclase, prehnite, and one white mineral. Bastite is composed of serpentine. Spinel looks fresh. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins."	"Protogranular serpentinized harzburgite with rare patchy regular mesh. Irregular dunite layer with a gently dipping contacteveral magmatic veins with moderate dips cut by green veins.  "	
"399"	"U1601"	"C"	"59"	"R"	"3"	""	"399-U1601C-59R-3"	"0.0"	"75.5"	"302.200"	"302.577"	"302.955"	"302.2"	"302.577"	"302.955"	""	"1"	""	"Harzburgite with a pyroxenite trail at c. 16 cm. below 41 cm is a 2 cm-wide vein of medium grained gabbronorite within dunite."	"Highly serpentinized harzburgite and minor dunite crosscut by two hydrothermally overprinted magmatic veins. The latter are made of chlorite, amphibole, secondary plagioclase, prehnite, and one pink mineral. Possible rodingite. Bastite is composed of serpentine. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins. The latter cut through the hydrothermally altered magmatic veins."	"Protogranular serpentinized harzburgite with no mesh, above dunite (contact dip 30°), with no mesh. Cut by several magmatic veins moderate dips, some branched, cut by green veins."	
"399"	"U1601"	"C"	"59"	"R"	"4"	""	"399-U1601C-59R-4"	"0.0"	"113.0"	"302.955"	"303.520"	"304.085"	"302.955"	"303.52"	"304.085"	""	"1"	""	"The dunite from the previous section continues here to 7.4 cm. Harzburgite is beneath with interspersed gabbronorite patches and veins."	"Highly serpentinized harzburgite and minor dunite crosscut by two hydrothermally altered magmatic veins. The latter is made of chlorite, amphibole, secondary plagioclase, prehnite, and one pink mineral. Possible rodingite. Bastite is composed of serpentine and the color changes from black-green-white to green-black-white down section. The serpentinite is cut by several types of veins including serpentine-magnetite veins forming mesh and a network of fibrous to massive chrysotile veins."	"Thin dunite interval above protogranular serpentinized harzburgite with a moderately dipping contact, and regular to no mesh.  Magmatic veins with moderate dips and little white veins that are shallowly dipping."	
"399"	"U1601"	"C"	"60"	"R"	"1"	""	"399-U1601C-60R-1"	"0.0"	"147.0"	"304.300"	"305.035"	"305.770"	"304.3"	"305.035"	"305.77"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with horizons of orthopyroxene-bearing dunite associated with two multiple-cm-scale gabbroic veins. One centered at 24 cm is coarse-grained gabbro with finer-grained margins. The second is a coarse-grained gabbronorite centered at 102 m."	"Highly serpentinized harzburgite and minor dunite. The latter is crosscut by two hydrothermally altered magmatic veins. The magmatic veins are made of amphibole after clinopyroxene, and secondary plagioclase, chlorite, and prehnite after plagioclase. Bastite is composed of serpentine. The serpentinized harzburgite and dunite are cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, and massive green picrolite veins. The picrolite veins cut through the hydrothermally altered magmatic veins."	"Protogranular serpentinized harzburgite with regular mesh.  Dunite interval has regular mesh, intruded by magmatic vein.  Thin isotropic gabbro intervals, with moderately dipping contacts.  White and green veins with moderate dip (30-40°)."	
"399"	"U1601"	"C"	"60"	"R"	"2"	""	"399-U1601C-60R-2"	"0.0"	"147.0"	"305.770"	"306.505"	"307.240"	"305.77"	"306.505"	"307.24"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Harzburgite with dunite intervals in the upper 35 cm. A highly altered gabbroic vein with sulfides is centered 84 cm. It is bounded by orthopyroxene-bearing dunite. The lowermost piece is medium-grained olivine gabbro."	"Highly serpentinized harzburgite and minor Opx-bearing dunite; the latter is crosscut by two hydrothermally altered magmatic veins. The magmatic veins are composed of amphibole after clinopyroxene, and secondary plagioclase, chlorite, and prehnite after plagioclase. There is a small gabbro pebble at the bottom of the section (144-147 cm). Bastite is composed of serpentine. Locally, sulfides are associated with bastite. The serpentinites are cut by several types of veins including serpentine-magnetite veins forming mesh, a network of fibrous to massive chrysotile veins, massive green picrolite veins, and massive clay-carbonate veins."	"Protogranular serpentinized harzburgite with regular to no mesh. Dunite interval with an irregular, moderately dipping contact.  Magmatic veins with moderate dip, gray and white veins with moderate dip.  Little white veins with shallow dip."	
"399"	"U1601"	"C"	"60"	"R"	"3"	""	"399-U1601C-60R-3"	"0.0"	"125.0"	"307.240"	"307.865"	"308.490"	"307.24"	"307.865"	"308.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Medium-grained seriate olivine gabbro with grain sizes varying down section. Abundant Cu-Zn-Fe sulfides are present within the interval of 6.5-12cm."	"Hydrothermally altered coarse-grained gabbro, locally forming greenstone. At the top of the section, there is relatively fresh gabbro. Massive sulfides (chalcopyrite/pyrrhotite?) are associated with carbonates (7-12 cm). In gabbro, amphibole forms after clinopyroxene, and chlorite, prehnite and secondary plagioclase form after plagioclase. The gabbro is cut by two chlorite veins."	"Isotropic, altered green gabbro (undeformed), with grain size variations.  Green and white veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"61"	"R"	"1"	""	"399-U1601C-61R-1"	"0.0"	"150.0"	"309.200"	"309.950"	"310.700"	"309.2"	"309.95"	"310.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Mostly fine to coarse grained seriate olivine gabbro. Some patches are troctolitic (e.g. interval 15-18). Clinopyroxene ranges from granular to poikilitic with grain sizes varying from 1 mm to >50mm to multi-cm scale grains. The top-most piece is a deformed harzburgite."	"Variably altered gabbro, locally forming greenstone. In gabbro, amphibole after clinopyroxene, and chlorite, prehnite and secondary plagioclase after plagioclase. The gabbro is cut by quartz-sulfide and chlorite veins."	"Isotropic gabbro with shallow to steeply dipping grain size and modal layering. One interval fractured. Small serpentinized harzburgite rubble near the top."	
"399"	"U1601"	"C"	"61"	"R"	"2"	""	"399-U1601C-61R-2"	"0.0"	"118.0"	"310.700"	"311.290"	"311.880"	"310.7"	"311.29"	"311.88"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Olivine gabbro continued from the overlying section, but less variable in grain size. This gabbro is medium grained, and its texture is granular thoughout. Olivine proportions are relatively constant. at 15%. Piece 9 has opx."	"Variably altered Ol-bearing gabbro, locally forming greenstone. In gabbro, amphibole forms after clinopyroxene, and chlorite and secondary plagioclase form after plagioclase. Olivine is altered to serpentine and magnetite and possibly amphibole and talc. The gabbro is cut by several types of veins including amphibole, chlorite-clay veins, and quartz veins."	"Isotropic, undeformed gabbro with modal and grain size layering (45° dip), cut by  green, black and quartz veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"61"	"R"	"3"	""	"399-U1601C-61R-3"	"0.0"	"97.0"	"311.880"	"312.365"	"312.850"	"311.88"	"312.365"	"312.85"	""	"1, 2, 3, 4"	""	"Olivine gabbro with mineral abundances that are similar to overlying sections, but with overall finer grain sizes. "	"Slightly altered Ol-bearing gabbro. Amphibole forms after clinopyroxene, and chlorite and secondary plagioclase form after plagioclase. This section is fresher than 61R-2. It is cut by several types of veins including amphibole, and haloed chlorite veins."	"Isotropic, undeformed gabbro with modal and grainsize layering (45° dip). One interval with a weak SPO defined by clinopyroxene with moderate dip.  Cut by magmatic vein with moderate dip, black, green, white veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"61"	"R"	"4"	""	"399-U1601C-61R-4"	"0.0"	"71.0"	"312.850"	"313.205"	"313.560"	"312.85"	"313.205"	"313.56"	""	"1, 2, 3, 4"	""	"Olivine gabbro continued from overlying sections. Grain size is greater and olivine proportions are lower compared with the overlying section."	"Variably altered Ol-bearing gabbro, locally forming greenstone. Amphibole forms after clinopyroxene, and chlorite and secondary plagioclase form after plagioclase. Gabbro is cut by three chlorite-clay veins."	"Isotropic gabbro, undeformed with moderat dip irregular grain size and modal variations; cut by magmatic veins, in turn cut by green veins."	
"399"	"U1601"	"C"	"62"	"R"	"1"	""	"399-U1601C-62R-1"	"0.0"	"142.0"	"314.000"	"314.710"	"315.420"	"314"	"314.71"	"315.42"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Olivine gabbro continues unabated to 46 cm, where the olivine disappears and the rock type becomes a coarse grained gabbro down to a contact 63 cm. The contact is riddled with veins of secondary minerals. Intermingled harzburgite and coarse-grained gabbro domains are beneath this contact. "	"Variably altered Ol-bearing gabbro. Amphibole replaces clinopyroxene, and chlorite and secondary plagioclase replace plagioclase. Gabbro is cut by several types of veins including amphibole, chlorite-zeolite, carbonate-zeolite-clay vein that overprint plagioclase-prehnite veins. Clay-zeolite veins form sets or networks."	"Isotropic gabbro with grain size and modal variations in contact with protogranular serpentinized harzburgite, with no mesh. Contact is a fault parallel by thick white vein with slickenfibres suggesting reverse motion.  Cut by several black, green, white veins with shallow to steep dips."	
"399"	"U1601"	"C"	"62"	"R"	"2"	""	"399-U1601C-62R-2"	"0.0"	"142.5"	"315.420"	"316.132"	"316.845"	"315.42"	"316.132"	"316.845"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The first piece is a highly altered gabbro. Harzburgite with trace spinel is beneath, with rare interspersed altered gabbro veins."	"Highly serpentinized harzburgite and minor dunite. The harzburgite is cut by one hydrothermally altered magmatic vein. Gabbro occurs at the top of the section (0-8.5 cm). Gabbro is altered to amphibole after clinopyroxene and chlorite and secondary plagioclase (and possibly prehnite) after plagioclase. Bastite is composed of serpentine. Spinel looks fresh. The serpentinized peridotites are crosscut by several types of veins including mesh, chrysotile, and carbonate-clay veins locally overprinting or crosscutting the magmatic veins. Gabbro is cut by carbonate-zeolite and amphibole veins."	"Protogranular serpentinized harzburgite with regular mesh. Magmatic veins with moderate dip, white, green, and gray veins with shallow to moderate dips. 0-9cm has dense vein network of qtz veins + sulphides in serpentinite."	
"399"	"U1601"	"C"	"62"	"R"	"3"	""	"399-U1601C-62R-3"	"0.0"	"124.0"	"316.845"	"317.465"	"318.085"	"316.845"	"317.465"	"318.085"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with trace spinel. Contains a 2 cm thick highly altered gabbro vein centered at 25 cm."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veins. The latter is made of amphibole after clinopyroxene, and chlorite, secondary plagioclase, and possibly prehnite after plagioclase. Bastite is composed of serpentine. Spinel looks fresh. Several types of veins crosscut the serpentinized harzburgite including mesh, chrysotile, and late carbonate-clay veins. Zeolite veins cut through the magmatic veins and extend to picrolite further away from the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh. Cut by magmatic veins (moderate dip), and white and green veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"63"	"R"	"1"	""	"399-U1601C-63R-1"	"0.0"	"133.0"	"318.900"	"319.565"	"320.230"	"318.9"	"319.565"	"320.23"	""	"1, 2"	""	"Harzburgite with mostly granular orthopyroxene and two 1-2mm thick veins of gabbro down to 107 cm. Beneath 107 cm is an orthopyroxene-bearing dunite containing a highly deformed and altered gabbroic vein centered at 119 cm. The dunite has some clinopyroxene near the border of the gabbro vein."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veins. The latter is made of amphibole after clinopyroxene, and chlorite, secondary plagioclase, and possibly prehnite after plagioclase. Bastite is composed of serpentine. Several types of veins crosscut the serpentinized harzburgite including mesh and chrysotile veins. Zeolite-carbonate-clay veins cut through the magmatic veins and extend to picrolite further away from the magmatic veins."	"Protogranular serpentinized harzburgite with no to regular mesh. Cut by magmatic veins (moderate dip). "	
"399"	"U1601"	"C"	"63"	"R"	"2"	""	"399-U1601C-63R-2"	"0.0"	"133.5"	"320.230"	"320.897"	"321.565"	"320.23"	"320.897"	"321.565"	""	"1"	""	"Harzburgite with mostly granular orthopyroxene and with a few 1-10 mm thick gabbroic veins scatted down the core. "	"Highly serpentinized harzburgite and Opx-bearing dunite cut by four hydrothermally altered magmatic veins. Pebbles of altered gabbro at the bottom of the section. Gabbro is made of amphibole, secondary plagioclase, chlorite, and possibly prehnite. The hydrothermally overprinted magmatic veins are made of amphibole after clinopyroxene, and chlorite, secondary plagioclase, and possibly prehnite after plagioclase. Bastite is composed of serpentine. Several types of veins crosscut the serpentinized harzburgite including mesh and chrysotile veins. Carbonate-clay and chrysotile veins cut through the magmatic veins. At the contact between the gabbro and the serpentinized peridotite, a vein containing an unidentified white mineral (hardness between 2 and 3) is present."	"Protogranular serpentinized harzburgite with regular pathcy mesh. Cut by magmatic veins (moderate dip), and white, red and green veins."	
"399"	"U1601"	"C"	"63"	"R"	"3"	""	"399-U1601C-63R-3"	"0.0"	"150.0"	"321.565"	"322.315"	"323.065"	"321.565"	"322.315"	"323.065"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Two domains running much of the length of the core: (1) Highly altered, bleached harzburgite with both granular and interstitial orthopyroxene. Bleaching is centered between 81 and 112 cm. (2) Coarse-grained granular gabbro with sharp but sutured contact with harzburgite."	"Contact between highly serpentinized harzburgite and altered gabbro (dominant). The contact is highly metasomatized with abundant prehnite, chlorite, and secondary plagioclase. Gabbro is made of amphibole after clinopyroxene, secondary plagioclase, chlorite, and possibly prehnite and zeolite after plagioclase. Prehnite is dominant at the contact between gabbro and the peridotite and its abundance decreases in the gabbro away from the contact. The harzburgite is highly metasomatized and appears green to grey, the mesh is not visible. Bastite is composed of serpentine. The harzburgite is cut by several types of veins including prehnite-zeolite veins, picrolite veins, chrysotile veins, and late carbonate veins. Except for chrysotile, all the vein types contain Cu-sulfides (possibly chalcopyrite and bornite). Prehnite-zeolite-sulfide vein occurs at the contact between green and grey harzburgite and is cut by massive picrolite-sulfide veins. Gabbro is cut by chlorite, clays, and zeolite veins."	"Steeply dipping contact between serpentinized harzburgite and gabbro. Gabbro is strongly altered and isotropic. Moderate dip green veins cut contact."	
"399"	"U1601"	"C"	"64"	"R"	"1"	""	"399-U1601C-64R-1"	"0.0"	"150.0"	"323.700"	"324.450"	"325.200"	"323.7"	"324.45"	"325.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Coarse-grained granular gabbro continuous with 63R-3 at the intervals of 0-60 cm and 102-138cm . Harzburgite with trace spinel is between 60 and 101 cm. Orthopyroxene-bearing dunite is below 137 cm."	"Contact between highly serpentinized Opx-bearing dunite and altered gabbro (dominant). The contact is highly metasomatized with abundant prehnite, chlorite, and secondary plagioclase. Gabbro is made of amphibole after clinopyroxene, and secondary plagioclase, chlorite, and possibly prehnite and zeolite after plagioclase. Prehnite is dominant at the contact between the gabbro and the peridotite and its abundance decreases in the gabbro away from the contact. The Opx-bearing dunite is highly metasomatized and appears green to grey. The mesh is not visible. Bastite is composed of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, chrysotile, and picrolite-sulfide veins. The latter cut chrysotile veins In the gabbro, veins made of chlorite-clay, zeolite, and secondary plagioclase-chlorite are observed."	"Protogranular serpentinized harzburgite with no mesh, between altered gabbroic intervals (contact dips 55°).  Cut by green, grey, and white veins with moderate dips."	
"399"	"U1601"	"C"	"64"	"R"	"2"	""	"399-U1601C-64R-2"	"0.0"	"137.0"	"325.200"	"325.885"	"326.570"	"325.2"	"325.885"	"326.57"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Coarse-grained seriate gabbro down to 103 cm with compositions similar to gabbros in 63R-3 and 64R-1. Pure dunite is beneath the gabbro, which grades to a harzburgite beginning at 109 cm."	"Gabbro (altered) contact with minor serpentinized dunite and harzburgite. Cu-sulfides are present in the gabbro. The serpentinized peridotite is cut by serpentine-magnetite, chrysotile, and composite picrolite-chrysotile veins. In the gabbro, zeolite-clay and chlorite veins are observed."	"Altered, undeformed isotropic gabbro, above dunite and serpentinized protogtranular harzburgite, with patchy regular mesh.  Cut by gently dipping veins."	
"399"	"U1601"	"C"	"65"	"R"	"1"	""	"399-U1601C-65R-1"	"0.0"	"133.0"	"328.600"	"329.265"	"329.930"	"328.6"	"329.258"	"329.916"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite in sharp contact with a 8 mm thick gabbronorite vein centered at 107 cm. Orthopyroxene proportions in the harzburgite diminish near the vein. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. The hydrothermally overprinted magmatic vein is composed of amphibole, chlorite, secondary plagioclase, prehnite, and a pink mineral. The serpentinized peridotite is cut by serpentine-magnetite and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with no to regular mesh, cut by magmatic vein (moderately dipping), several white veins from gentle to steeply dipping, and subhorizontal little white veins."	
"399"	"U1601"	"C"	"65"	"R"	"2"	""	"399-U1601C-65R-2"	"0.0"	"140.0"	"329.930"	"330.630"	"331.330"	"329.916"	"330.609"	"331.302"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Harzburgite in sharp contact with a 1 cm thick gabbronorite vein centered at 80 cm. Orthopyroxene proportions in the harzburgite diminish near the vein. "	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. Spinel is fresh. Bastite locally features green corona. The hydrothermally overprinted magmatic vein is composed of amphibole, chlorite, secondary plagioclase, prehnite, and a pink mineral. The serpentinized peridotite is cut by chlorite, serpentine-magnetite, and fibrous to massive chrysotile veins. Where chrysotile cuts through the magmatic vein, it turns to picrolite."	"Protogranular serpentinized harzburgite with no to regular mesh, cut by magmatic vein (moderate to steep dip), and several white veins."	
"399"	"U1601"	"C"	"65"	"R"	"3"	""	"399-U1601C-65R-3"	"0.0"	"135.0"	"331.330"	"332.005"	"332.680"	"331.302"	"331.97"	"332.638"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with a highly altered gabbroic vein with a thickness of about 5 mm. This vein is centered at c. 50 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. Spinel is fresh. Bastite locally features green corona. The hydrothermally overprinted magmatic vein is composed of amphibole, chlorite, secondary plagioclase, prehnite, a pink mineral, and possibly clinopyroxene. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and massive serpentine veins."	"Protogranular serpentinized harzburgite with patchy regular mesh, cut by magmatic vein (moderately dipping), and shallow to moderately dipping white veins."	
"399"	"U1601"	"C"	"65"	"R"	"4"	""	"399-U1601C-65R-4"	"0.0"	"77.0"	"332.680"	"333.065"	"333.450"	"332.638"	"333.019"	"333.4"	""	"1, 2, 3"	""	"Harzburgite with a 5 mm wide, highly altered gabbroic vein at the end of the section. The harzburgite has scattered dunitic patches. "	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. Spinel is fresh. Bastite locally features green corona. The hydrothermally overprinted magmatic vein is composed of amphibole, chlorite, secondary plagioclase, prehnite, a pink mineral, and possibly clinopyroxene. The serpentinized peridotite is cut serpentine-magnetite, fibrous to massive chrysotile. Zeolite-chlorite veins cut through the hydrothermally overprinted magmatic vein."	"Protogranular serpentinized harzburgite with regular mesh, cut by a gently dipping magmatic vein, and 10-30° dipping white veins. "	
"399"	"U1601"	"C"	"66"	"R"	"1"	""	"399-U1601C-66R-1"	"0.0"	"150.0"	"333.400"	"334.150"	"334.900"	"333.4"	"334.15"	"334.9"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with minor clinopyroxene. It has two thin gabbro veins centered at 36 and 120 cm. An olivine-bearing gabbro pebble is at c. 28 cm. The olivine in this pebble was probably derived from the host harzburgite."	"Highly serpentinized harzburgite cut by three hydrothermally altered magmatic veins. One piece of diorite (27-30 cm). The hydrothermally overprinted magmatic veins are composed of amphibole, chlorite, secondary plagioclase, and prehnite. The serpentinized harzburgite is cut by several types of veins including serpentine-magnetite, fibrous to massive chrysotile, and picrolite veins. The latter also cut through the magmatic veins."	"Protogranular serpentinized harzburgite with patchy regular mesh, cut by two moderately dipping magmatic veins, and  0-25 deg dipping white veins."	
"399"	"U1601"	"C"	"66"	"R"	"2"	""	"399-U1601C-66R-2"	"0.0"	"141.0"	"334.900"	"335.605"	"336.310"	"334.9"	"335.605"	"336.31"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The top 70 cm is harzburgite with scattered olivine-bearing gabbro veins. From 70 to 105 cm is a coarse-grained to pegmatitic olivine bearing gabbro. This gabbro is in sharp contact with the underlying harzburgite, which has relatively low modal orthopyroxene."	"Highly serpentinized harzburgite and minor dunite; the harzburgite is cut by hydrothermally altered magmatic veins. Altered gabbro intrusion (69-105 cm). Amphibole after clinopyroxene, chlorite, secondary plagioclase, and prehnite after plagioclase. The hydrothermally overprinted magmatic veins are composed of amphibole, chlorite, secondary plagioclase, and prehnite. The serpentinized peridotites are cut by several types of veins including serpentine-magnetite, fibrous to massive chrysotile, and picrolite veins. The latter also cut through the magmatic veins. Gabbro is crosscut by a set of chlorite-clay and zeolite veins."	"Protogranular serpentinized harzburgite with weakly foliated to patchy regular mesh. isotropic gabbro with moderately dipping upper contact and shallowly dipping lower contact.  Several magmatic veins, moderately dipping.  Several white veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"66"	"R"	"3"	""	"399-U1601C-66R-3"	"0.0"	"91.0"	"336.310"	"336.765"	"337.220"	"336.31"	"336.765"	"337.22"	""	"1, 2, 3, 4, 5, 6"	""	"Good example of "black harzburgite." This particular harzburgite has a relatively low orthopyroxene abundance. The orthopyroxene is nearly invisible against the black serpentinized olivine as a result of its own alteration to a similar black color."	"Highly serpentinized Opx-bearing dunite cut by one hydrothermally altered magmatic vein. The hydrothermally overprinted magmatic veins are composed of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. The dunite appears brown-stained and contains disseminated sulfides and small sulfides veinlets. Bastite is composed of serpentine. The serpentinized dunite is cut by several types of veins including serpentine-magnetite, rare fibrous chrysotile, picrolite-Cu-sulfides, and late carbonate-Cu-sulfide veins. Picrolite-Cu-sulfide cut through the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh, cut by a moderately dipping magmatic vein, and gently dipping grey-orange veins."	
"399"	"U1601"	"C"	"67"	"R"	"1"	""	"399-U1601C-67R-1"	"0.0"	"140.0"	"338.300"	"339.000"	"339.700"	"338.3"	"339"	"339.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The upper 41 cm is highly altered gabbro hosted in dunite to harzburgite with minimal orthopyroxene. The boundary between these domains is troctolitic. Clinopyroxene-bearing harzburgite lies beneath. Clinopyroxene is particularly evident from 60 to 73 cm."	"Serpentinized harzburgite and highly altered gabbro. Serpentinized harzburgite is cut by an altered magmatic vein composed of secondary plagioclase, prehnite, chlorite, and opaque minerals. A small troctolite layer is almost completely altered. Troctolite contains disseminated sulfides. Gabbro is altered to greenstone. The serpentinized harzburgite is cut by several types of veins including serpentine-magnetite, and (few) fibrous to massive chrysotile veins. The latter also cut through hydrothermally overprinted magmatic veins. Prehnite-carbonate-chlorite-sulfide veins cut through the gabbro."	"Isotropic gabbro, with 45° dipping contacts to protogranular, serpentinized harzburgite with regular mesh; cut by subhorizontal and moderately dipping white veins."	
"399"	"U1601"	"C"	"67"	"R"	"2"	""	"399-U1601C-67R-2"	"0.0"	"145.0"	"339.700"	"340.425"	"341.150"	"339.7"	"340.425"	"341.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Harzburgite relatively poor in orthopyroxene hosting a leucocratic gabbroic domain from 39 to 70 cm, and a 1 cm gabbroic vein centered at 135 cm."	"Serpentinized harzburgite cut by three hydrothermally overprinted magmatic veins. Highly altered and bleached magmatic interval composed of amphibole, secondary plagioclase, chlorite, prehnite, and possibly zeolite. Carbonate occurs at the contact with harzburgite. The serpentinized harzburgite is cut serpentine-magnetite and a few fibrous to massive chrysotile veins. The latter also cut through hydrothermally overprinted magmatic veins. The gabbro is cut by zeolite-clay and carbonate veins grading to picrolite when propagating in the serpentinized harzburgite."	"Protogranular serpentinized harzburgite with gabbro interval, contact moderately dipping.  Cut by magmatic vein, moderately dipping, then white, brown, and green veins the have moderate dips."	
"399"	"U1601"	"C"	"68"	"R"	"1"	""	"399-U1601C-68R-1"	"0.0"	"111.5"	"343.100"	"343.658"	"344.215"	"343.1"	"343.652"	"344.204"	""	"1, 2, 3, 4, 5, 6"	""	"Accidental pebbles of gabbro at a the top. The rest of the section is harzburgite with trace clinopyroxene and spinel."	"Highly serpentinized harzburgite. Piece of altered gabbro at the top of the section (0-7 cm). The gabbro is variably altered to amphibole, secondary plagioclase, chlorite, prehnite. In serpentinized harzburgite, bastite is composed of serpentine. The serpentinized harzburgite is cut by serpentine-magnetite, few fibrous to late massive chrysotile, and late serpentine-carbonate veins (that cut all mentioned earlier veins). The gabbro is cut by zeolite and amphibole veins."	"Protogranular serpentinized harzburgite with gabbro interval. Little white veins vary in dip from 0 to 25 deg.  Cut by several white and green veins, one is a piece end fault."	
"399"	"U1601"	"C"	"68"	"R"	"2"	""	"399-U1601C-68R-2"	"0.0"	"146.0"	"344.215"	"344.945"	"345.675"	"344.203"	"344.925"	"345.646"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with trace clinopyroxene down to 85 cm. The central part of the section is domains of gabbro and olivine-rich troctolite. Beneath 104 cm is harzburgite with a few cm-scale veins of secondary minerals."	"Highly serpentinized harzburgite and dunite. The latter is cut by a hydrothermally altered magmatic vein. Variably altered gabbro. The gabbro is altered to amphibole, secondary plagioclase, chlorite, and prehnite. The hydrothermally overprinted magmatic veins are composed of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. In serpentinized harzburgite, bastite is composed of serpentine. The serpentinized harzburgite is cut by serpentine-magnetite, fibrous to late massive chrysotile veins, and late carbonate veins that cut through chrysotile veins. The magmatic vein is overprinted by carbonate and zeolite. The gabbro is cut by chlorite and zeolite veins."	"Protogranular serpentinized harzburgite with isotropic modal layered gabbro."	
"399"	"U1601"	"C"	"68"	"R"	"3"	""	"399-U1601C-68R-3"	"0.0"	"140.5"	"345.675"	"346.377"	"347.080"	"345.646"	"346.349"	"347.051"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Most of the section consists of harzburgite with trace spinel. A medium grained gabbro unit with grain sizes increasing toward its center and with some xenolithic olivine at its boundary is present between 74 and 93 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite. Variably altered gabbro. The gabbro is altered to amphibole, secondary plagioclase, chlorite, and prehnite. In serpentinized peridotites, bastite is made of serpentine. The serpentinized peridotites are cut by serpentine-magnetite veins, fibrous chrysotile veins, massive serpentine-sulfides veins, and carbonate-sulfides veins. The gabbro is cut by zeolite and chlorite veins."	"Serpentinized harzburgite with no mesh and gabbro interval."	
"399"	"U1601"	"C"	"68"	"R"	"4"	""	"399-U1601C-68R-4"	"0.0"	"97.5"	"347.080"	"347.567"	"348.055"	"347.036"	"347.519"	"348.001"	""	"1, 2"	""	"Garden variety harzburgite with a few 1 mm scale altered veins centered at 44, 80, and 85.5 cm. "	"Almost completely serpentinized harzburgite with one hydrothermally altered magmatic patch/vein. The latter is altered to amphibole and chlorite. In serpentinized peridotite, bastite is made of serpentine. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous chrysotile veins, and a set of 3 veins made of a white mineral associated with magnetite."	"Protogranular serpentinized harzburgite with a regular to weak mesh."	
"399"	"U1601"	"C"	"69"	"R"	"1"	""	"399-U1601C-69R-1"	"0.0"	"142.0"	"348.000"	"348.710"	"349.420"	"348"	"348.704"	"349.408"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Accidental pebbles of harzburgite and olivine gabbro through 12 cm. The rest of the section is harzburgite. Its orthopyroxene content decreases down section from c. 15 at the top to c. 10 % at the base."	"Highly serpentinized harzburgite. A small piece of gabbro at the top of the section is moderately altered to amphibole after clinopyroxene, and chlorite and secondary plagioclase after plagioclase. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous chrysotile veins, and massive chrysotile veins. The fibrous chrysotile cuts the massive chrysotile veins. Amphibole veins occur in the gabbro."	"Protogranular to porphyroclastic serpentinized harzburgite with regular mesh to no mesh and little white veins."	
"399"	"U1601"	"C"	"69"	"R"	"2"	""	"399-U1601C-69R-2"	"0.0"	"139.0"	"349.420"	"350.115"	"350.810"	"349.408"	"350.098"	"350.787"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The top 30 cm is olivine-b gabbro with a coarse-grained core and a finer olivine-rich reaction boundary towards the harzburgite host. The remainder of the section is harzburgite containing gabbro veins 1-6 cm thick that are sheared and altered to the point that the primary mineral characteristics are obscured. The primary gabbro veins are centered at 85 cm and 100 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Variably altered gabbro up-section, to amphibole after clinopyroxene, chlorite, prehnite, and secondary plagioclase after plagioclase. The hydrothermally overprinted magmatic vein is composed of prehnite, carbonates, opaque minerals, and a light cream mineral. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite and fibrous chrysotile veins. The gabbro is cut by a set of chlorite and one prehnite veins."	"Coarse pegmatitic gabbro, undeformed, isotropic, above protogranular to porphyroclastic serpentinized harzburgite, cut by several veins."	
"399"	"U1601"	"C"	"69"	"R"	"3"	""	"399-U1601C-69R-3"	"0.0"	"122.0"	"350.810"	"351.420"	"352.030"	"350.787"	"351.392"	"351.997"	""	"1, 2, 3, 4"	""	"Harzburgite with a trace of clinopyroxene."	"Highly serpentinized harzburgite. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and late carbonate veins."	"Protogranular to porphyroclastic (subhorizontal) to protogranular serpentinized harzburgite with regular mesh cut by subhorizontal little white veins."	
"399"	"U1601"	"C"	"69"	"R"	"4"	""	"399-U1601C-69R-4"	"0.0"	"81.0"	"352.030"	"352.435"	"352.840"	"351.997"	"352.399"	"352.8"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with three veins < 1 mm in width and of unknown origin."	"Highly serpentinized harzburgite. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite and fibrous to massive chrysotile veins."	"Protogranular to porphyroclastic (10° dip) to protogranular serpentinized harzburgite with regular mesh, cut by 25° dipping little white veins."	
"399"	"U1601"	"C"	"70"	"R"	"1"	""	"399-U1601C-70R-1"	"0.0"	"128.0"	"352.800"	"353.440"	"354.080"	"352.8"	"353.428"	"354.057"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"The first piece is an olivine gabbro pebble, probably of accidental origin. The rest of the section is harzburgite with trace spinel and varying orthopyroxene proportions. The proportions generally decrease down section."	"Highly serpentinized harzburgite. The top of the section is made of a small piece of gabbro altered to amphibole after clinopyroxene, and chlorite and secondary plagioclase after plagioclase. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and late massive chrysotile veins."	"Porphyroclastic (20° dip) serpentinized harzburgite with regular mesh, cut by 20° dipping little white veins."	
"399"	"U1601"	"C"	"70"	"R"	"2"	""	"399-U1601C-70R-2"	"0.0"	"146.0"	"354.080"	"354.810"	"355.540"	"354.057"	"354.774"	"355.491"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with trace spinel and orthopyroxene proportions varying from 12-20%."	"Highly serpentinized Opx-bearing dunite. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and massive picrolite veins."	"Porphyroclastic (5° dip) to protogranular serpentinized harzburgite with regular mesh, cut by 5° dipping little white veins."	
"399"	"U1601"	"C"	"70"	"R"	"3"	""	"399-U1601C-70R-3"	"0.0"	"128.0"	"355.540"	"356.180"	"356.820"	"355.491"	"356.12"	"356.748"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with a prominent vein of coarse grained gabbro between 28 and 33 cm. The remainder of the section has diffuse gabbro impregnations, some of which mix with peridotite to give a plagioclase lherzolite mineralogy. The bottom pebble is medium-grained gabbro."	"Highly serpentinized harzburgite, with a variable abundance of orthopyroxene, cut by a set of hydrothermally altered magmatic veins. The latter are made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Bastite is made of serpentine and talc. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins that cut chrysotile veins, small sulfides veinlets, and massive and composite serpentine-carbonate veins."	"Protogranular serpentinized harzburgite with weak subhorizontal mesh foliation and gabbro intervals. Gabbro interval is protomylonite, other magmatic veins are isotropic, including pyrite in matrix. Protomylonite is cut by undeformed white vein."	
"399"	"U1601"	"C"	"70"	"R"	"4"	""	"399-U1601C-70R-4"	"0.0"	"97.0"	"356.820"	"357.305"	"357.790"	"356.748"	"357.224"	"357.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Harzburgite above orthopyroxene-bearing dunite down to 80 cm. The dunite hosts two c, 1 cm thick gabbronorite vein centered at 72.5 cm and 78.5 cm."	"Highly serpentinized Opx-bearing dunite cut by one hydrothermally altered magmatic vein. The latter is made of primary clinopyroxene and plagioclase and secondary amphibole, plagioclase, chlorite, and prehnite. Bastite is composed of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins, small sulfides veinlets locally associated with serpentine, massive and composite serpentine-carbonate veins, and carbonate veins."	"Protogranular to porphyroclastic serpentinized harzburgite with no mesh."	
"399"	"U1601"	"C"	"71"	"R"	"1"	""	"399-U1601C-71R-1"	"0.0"	"150.0"	"357.700"	"358.450"	"359.200"	"357.7"	"358.45"	"359.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"The top 88 cm are domains of opx-bearing dunite and coarse grained gabbro.  Beneath 88 cm is a harzburgite."	"Highly serpentinized Opx-bearing dunite and hydrothermally altered gabbro. The latter is composed of primary clinopyroxene and plagioclase, as well as secondary amphibole, chlorite, and prehnite. Some of the orthopyroxene is completely altered to black bastite composed of serpentine. The mesh shows brown staining. The serpentinized peridotite is cut serpentine-magnetite, composite chrysotile-carbonate veins that locally only contain fibrous to massive chrysotile, and carbonate-serpentine veins that progressively grade to zeolite when cutting the magmatic veins."	"Protogranular serpentinized harzburgite with a regular mesh, cut by subvertical magmatic veins and several white-green veins."	
"399"	"U1601"	"C"	"71"	"R"	"2"	""	"399-U1601C-71R-2"	"0.0"	"145.0"	"359.200"	"359.925"	"360.650"	"359.2"	"359.925"	"360.65"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The harzburgite from the section above continues throughout this section. Gabbro domains are present at c. 10 cm and from 79-136 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins and hydrothermally altered gabbro. The latter and the magmatic vein are made of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, secondary plagioclase, prehnite, and zeolite. Some of the orthopyroxene is completely altered to black bastite composed of serpentine. The mesh shows brown staining. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and composite chrysotile-carbonate veins. The gabbro is cut by amphibole veins and chlorite veins."	"Protogranular to porphyroclastic serpentinized harzburgite with weakly foliated mesh. Cut by gabbro intervals which are undeformed but very altered, with moderate dips."	
"399"	"U1601"	"C"	"71"	"R"	"3"	""	"399-U1601C-71R-3"	"0.0"	"103.0"	"360.650"	"361.165"	"361.680"	"360.65"	"361.165"	"361.68"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Harzburgite with slightly more orthopyroxene compared with the previous section."	"Highly serpentinized harzburgite. Bastite is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and massive white serpentine veins."	"Protogranular to porphyroclastic (horizontal) serpentinized harzburgite with no mesh, cut by shallow dip little white veins."	
"399"	"U1601"	"C"	"72"	"R"	"1"	""	"399-U1601C-72R-1"	"0.0"	"142.0"	"362.500"	"363.210"	"363.920"	"362.5"	"363.21"	"363.92"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Harzburgite with relatively low orthopyroxene concentration above 67 cm. Course-grained down to medium-grained gabbronorite is below."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic patches, forming a discontinuous vein. Highly altered gabbro. The latter is made of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, secondary plagioclase, and prehnite. The magmatic vein is made of chlorite and amphibole after clinopyroxene and sulfides. Bastite is composed of serpentine. The serpentinized peridotite is cut serpentine-magnetite, fibrous to massive chrysotile, and late massive chrysotile veins. The gabbro is crosscut by a set of chlorite veins and zeolite veins."	"Protogranular serpentinized harzburgite with no mesh. isotropic gabbro, with grain size variations, cut by possibly sheared magmatic  veins."	
"399"	"U1601"	"C"	"73"	"R"	"1"	""	"399-U1601C-73R-1"	"0.0"	"146.0"	"367.400"	"368.130"	"368.860"	"367.4"	"368.13"	"368.86"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"Black harzburgite with small piece of gabbro at 102-105 cm. The irregular contact between the lithologies is preserved."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein. The latter is composed of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, secondary plagioclase, and prehnite. Bastite is composed of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and late massive chrysotile and composite chrysotile-carbonate veins. The magmatic vein is crosscut by a set of chlorite veins."	"Protogranular serpentinized harzburgite with no to weakly foliated subhorizontal mesh. Isotropic gabbro, undeformed, with grainsize variations, and horizontal little white veins."	
"399"	"U1601"	"C"	"74"	"R"	"1"	""	"399-U1601C-74R-1"	"0.0"	"150.0"	"372.200"	"372.950"	"373.700"	"372.2"	"372.95"	"373.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26"	""	"Harzburgite with an interval of gabbronorite from 6 to 35 cm. Orthopyroxene proportions in harzburgite decrease towards the gabbroic domain."	"Highly serpentinized harzburgite and altered gabbro composed of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, and plagioclase. Bastite is cpmposed of serpentine and talc. The serpentinized peridotite is cut serpentine-magnetite, fibrous to massive chrysotile, and late composite chrysotile-carbonate veins. The gabbro is cut by a network of zeolite veins."	"Protogranular serpentinized harzburgite with no mesh; gabbro interval with microfaulting."	
"399"	"U1601"	"C"	"74"	"R"	"2"	""	"399-U1601C-74R-2"	"0.0"	"150.0"	"373.700"	"374.450"	"375.200"	"373.7"	"374.45"	"375.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Garden variety harzburgite  with vein consisting of secondary minerals in the bottommost piece."	"Highly serpentinized harzburgite and altered gabbro (at the bottom of the section, 142-150 cm) composed of primary clinopyroxene and plagioclase and secondary amphibole, chlorite and plagioclase. Bastite is composed of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and late massive chrysotile and composite chrysotile-carbonate veins. The gabbro is cut by chlorite veins and one composite zeolite-carbonate vein."	"Protogranular serpentinized harzburgite with regular mesh, cut by several thick white veins."	
"399"	"U1601"	"C"	"75"	"R"	"1"	""	"399-U1601C-75R-1"	"0.0"	"150.0"	"377.100"	"377.850"	"378.600"	"377.1"	"377.85"	"378.6"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"Section of harzburgite riddled with coarse-grained gabbro veins and domains down to 98 cm. Trace spinel."	"Highly serpentinized black harzburgite with low orthopyroxene content and altered gabbro (0-79 cm) composed of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, prehnite, talc, and plagioclase. The mesh is brown stained. Bastite is locally black and composed of serpentine. There is a large, slightly altered clinopyroxene crystal in the second last piece (120-130 cm). Sulfides occur locally along the edges of harzburgite pieces. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile, and late composite chrysotile-carbonate veins. The gabbro is cut by talc veins and a network of zeolite veins."	"Isotropic microfaulted gabbro cut by  gently dipping talc veins above protogranular serpentinized  harzburgite, cut by steeply dipping gabbro magmatic vein, cut by several green veins."	
"399"	"U1601"	"C"	"75"	"R"	"2"	""	"399-U1601C-75R-2"	"0.0"	"145.5"	"378.600"	"379.327"	"380.055"	"378.6"	"379.327"	"380.055"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Harzburgite with 12 % orthopyroxene and trace spinel"	"Highly serpentinized black harzburgite with low orthopyroxene content. Bastite is locally black and made of serpentine. The mesh is brown stained. The serpentinized peridotite is cut by several types of veins including mesh, fibrous to massive chrysotile, massive chrysotile veins, composite chrysotile-carbonate veins, polycrystalline chrysotile-carbonate-sulfide veins, and carbonate veins."	"Protogranular serpentinized harzburgite with regular to no mesh,  cut by white veins."	
"399"	"U1601"	"C"	"75"	"R"	"3"	""	"399-U1601C-75R-3"	"0.0"	"135.0"	"380.055"	"380.730"	"381.405"	"380.055"	"380.73"	"381.405"	""	"1, 2, 3, 4, 5, 6, 7, 8, 09, 10, 11, 12, 13, 14, 15"	""	"Harzburgite like overlying section, but with interval of dunite with 8 % chrome-spinel between 63 and 104 cm."	"Highly serpentinized black harzburgite with low orthopyroxene content and green dunite with oxidized chromitite layers. The mesh is brown stained. Bastite is locally black in the upper parts of this section and turns green in down-section. It is made of serpentine. The serpentinized peridotites are cut by serpentine-magnetite, fibrous to masive chrysotile, composite serpentine-magnetite veins, and composite sulfide-white mineral vein. The latter cut through the dunite."	"Protogranular serpentinized harzburgite with weakly foliated to no mesh, with interval of opx bearing dunite, gradational subhorizontal contacts; dunite has moderate serperpentine foliation (0-45° dip). "	
"399"	"U1601"	"C"	"76"	"R"	"1"	""	"399-U1601C-76R-1"	"0.0"	"107.0"	"381.900"	"382.435"	"382.970"	"381.9"	"382.435"	"382.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Harzburgite with a medium-grained gabbro vein centered at 56 cm."	"Highly serpentinized black harzburgite with low orthopyroxene content cut by one hydrothermally altered magmatic vein. Small pieces of gabbro at the top of the section (0-12 cm). The gabbro and the magmatic vein are made of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, prehnite, and plagioclase. The mesh is brown stained. Bastite is locally black and composed of serpentine. The serpentinized peridotites are cut by serpentine-magnetite, fibrous to massive chrysotile, massive chrysotile veins that cut the fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with black-brown colour and no mesh to patchy regular mesh. small gabbro rubble pieces cut by thin isotropic gabbro vein."	
"399"	"U1601"	"C"	"76"	"R"	"2"	""	"399-U1601C-76R-2"	"0.0"	"106.0"	"382.970"	"383.500"	"384.030"	"382.97"	"383.5"	"384.03"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Harzburgite with coarse grained gabbro veins and domains centered at 39, 49, and beneath 85 cm."	"Altered gabbro and highly serpentinized black-to-green harzburgite with low orthopyroxene content. The latter is cut by one hydrothermally altered magmatic vein. The gabbro and the magmatic vein are made of primary clinopyroxene and plagioclase and secondary amphibole, chlorite, prehnite, and plagioclase. Mesh is brown stained. Bastite is locally black and is made of serpentine. The gabbro is cut by chlorite, talc, and zeolite veins. The serpentinized peridotite is cut by serpentine-magnetite veins, chrysotile veins, composite carbonate-serpentine veins, sulfide veins, and composite sulfide-serpentine veins."	"Gabbro and serpentinized harzburgite rubble and rollers. Gabbro has microfaults. Unoriented pieces have serpentinie-gabbro contacts."	
"399"	"U1601"	"C"	"77"	"R"	"1"	""	"399-U1601C-77R-1"	"0.0"	"145.0"	"386.800"	"387.525"	"388.250"	"386.8"	"387.525"	"388.25"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27"	""	"Olivine gabbro is at the top of the section down to 8 cm. Coarse-grained gabbros are below down to 111 cm. Orthopyroxene appears to be present in the gabbro (gabbronorite) between 44 and 57 cm. Harzburgite with 12 % orthopyroxene and trace spinel make up the rest of the section."	"Variably altered Ol-bearing gabbro to gabbronorite and highly serpentinized black to green harzburgite. The gabbro/gabbronorite is made of orthopyroxene, clinopyroxene, and plagioclase, as well as secondary amphibole, chlorite, prehnite, plagioclase, serpentine, magnetite, and zeolite. The mesh is brown stained. Bastite is green and is made of serpentine. The gabbro is cut by chlorite, talc, and carbonate veins. The serpentinized peridotite is cut by several types of veins including mesh and fibrous to massive chrysotile veins."	"Isotropic gabbro with modal layers (45° dip) and fractures and many cross cutting green veins, above protogranular serpentinized harzburgite with patchy regular mesh."	
"399"	"U1601"	"C"	"77"	"R"	"2"	""	"399-U1601C-77R-2"	"0.0"	"145.0"	"388.250"	"388.975"	"389.700"	"388.25"	"388.975"	"389.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite that is unusually enriched in orthopyroxene. Also contains trace chromium spinel."	"Moderately serpentinized harzburgite with abundant unaltered olivine and orthopyroxene. It is cut by one hydrothermally altered magmatic vein. The latter is made of secondary plagioclase, amphibole, chlorite, prehnite, and possibly talc. Possibly primary polymineralic sulfides (chalcopyrite-pyrrhotite) are present and associated with orthopyroxene. Mesh is green, brown, and black. Bastite ranges in color from light green to olive green and is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and picrolite veins that seem connected to massive chrysotile veins. The latter also cut through the former magmatic vein."	"Strongly foliated porphyroclastic serpentinized harzburgite with large elongate opx. Mesh is absent in high- density opx regions."	
"399"	"U1601"	"C"	"77"	"R"	"3"	""	"399-U1601C-77R-3"	"0.0"	"150.0"	"389.700"	"390.450"	"391.200"	"389.7"	"390.45"	"391.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite that is unusually enriched in orthopyroxene. Cpx occurs throughout but concentrated in a band at 65 cm. Also contains trace chromium spinel and 2 % clinopyroxene."	"Moderately serpentinized harzburgite with abundant unaltered olivine and orthopyroxene. Possibly primary polymineralic sulfides (chalcopyrite-pyrrhotite) are present and associated with orthopyroxene. Mesh is green, brown, and black. Bastite ranges in color from light green to olive green and is made of serpentine and talc. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Weakly foliated porphyroclastic serpentinized harzburgite (0-30° dipping mantle fabric) with poorly developed mesh and parallel anastomosing little white veins."	
"399"	"U1601"	"C"	"78"	"R"	"1"	""	"399-U1601C-78R-1"	"0.0"	"141.0"	"391.600"	"392.305"	"393.010"	"391.6"	"392.305"	"393.01"	""	"1, 2, 3, 4, 5"	""	"The top 7 cm has pebbles of gabbro and peridotites that are likely accidental. The rest is harzburgite that is unusually enriched in orthopyroxene, and with 0.5 % clinopyroxene. Two generations of orthopyroxene are evident with the 2nd (interstitial) overgrowing the 1st (granular), although there are some zones where only granular opx is present. These have a fabric at an angle to the surrounding hzb."	"Moderately serpentinized harzburgite with abundant unaltered olivine and orthopyroxene. Mesh is green, brown, and black. Bastite ranges in color from light green to olive green and is made of serpentine. Spinel looks fresh. The extent of serpentinization varies notably throughout the section, with greener areas being more serpentinized (132-141 cm) vs. less serpentinized areas (117-131 cm). Serpentinization front? The serpentinized peridotite is cut by serpentine-magnetite sulfide, fibrous to massive chrysotile veins, and one composite picrolite-magnetite-sulfide vein."	"Strongly foliated porphyroclastic to protomylonitic serpentinized harzburgite with incipient mesh."	
"399"	"U1601"	"C"	"78"	"R"	"2"	""	"399-U1601C-78R-2"	"0.0"	"143.0"	"393.010"	"393.725"	"394.440"	"393.01"	"393.725"	"394.44"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The harzburgite continues from the overlying section down to a sharp contact at 26 cm, but orthopyroxenes are smaller and less abundant. Some zones with just granular orthopyroxenes are present. Chromium spinel-bearing dunite composes the rest of the section."	"Highly serpentinized dunite and harzburgite. Mesh is brown with thick black magnetite-serpentine veins. Bastite ranges in color from light green to grey and is made of serpentine and talc. The serpentinized peridotite is cut by serpentine-magnetite and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with incipient mesh above dunite w with moderately dipping sheared contact."	
"399"	"U1601"	"C"	"78"	"R"	"3"	""	"399-U1601C-78R-3"	"0.0"	"55.0"	"394.440"	"394.715"	"394.990"	"394.44"	"394.715"	"394.99"	""	"1, 2, 3, 4, 5, 6"	""	"Chromium spinel-bearing dunite."	"Highly serpentinized dunite. Mesh is brown with some thick black magnetite-serpentine veins. In addition, this section features few fibrous to massive chrysotile veins."	"Dunite pieces with regular mesh."	
"399"	"U1601"	"C"	"79"	"R"	"1"	""	"399-U1601C-79R-1"	"0.0"	"150.0"	"396.500"	"397.250"	"398.000"	"396.5"	"397.151"	"397.802"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Dunite with trace chromium spinel."	"Almost completely serpentinized dunite. Mesh is green, brown, and grey with thick black magnetite-serpentine veins. Spinel shows a yellow metallic sheen and is surrounded by a brown corona (possibly an oxidation rim). The serpentinized peridotite is cut by serpentine-magnetite veins, a few fibrous to massive chrysotile veins, and massive picrolite veins."	"Dunite with regular mesh, mesh domains 1-1.5cm thick may outline olivine grains."	
"399"	"U1601"	"C"	"79"	"R"	"2"	""	"399-U1601C-79R-2"	"0.0"	"150.0"	"398.000"	"398.750"	"399.500"	"397.802"	"398.453"	"399.104"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Dunite with trace chromium spinel. Spinel locally forms clusters."	"Almost completely serpentinized dunite. Mesh is green, brown, and grey. Spinel features a yellow metallic sheen and is surrounded by a brown corona (possibly oxidation rim). The serpentinized peridotite is cut by serpentine-magnetite, a few fibrous to massive chrysotile veins, and massive picrolite veins."	"Dunite, weakly foliated to mylonitic (subhorizontal), with weak to strong foliated mesh."	
"399"	"U1601"	"C"	"79"	"R"	"3"	""	"399-U1601C-79R-3"	"119.0"	"132.0"	"400.690"	"400.755"	"400.820"	"400.137"	"400.193"	"400.25"	""	"4, 5"	""	"Dunite with 1% chromium spinel."	"Almost completely serpentinized dunite. Mesh is green, brown, and grey. Spinel has a yellow metallic sheen and is surrounded by a brown corona (possibly an oxidation rim). The serpentinized peridotite is cut by serpentine-magnetite veins, a few fibrous to massive chrysotile veins, and massive picrolite veins."	"Strongly foliated (protomylonitic ?) dunite with strong, subhorizontal mesh foliation. "	
"399"	"U1601"	"C"	"79"	"R"	"4"	""	"399-U1601C-79R-4"	"0.0"	"121.0"	"400.820"	"401.425"	"402.030"	"400.25"	"400.775"	"401.3"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Dunite with 1% chromium spinel down to 55 cm. Harzburgite with granular and interstitial textures of orthopyroxene is below. The total orthopyroxene proportion is about 12%. A domain of medium- to coarse-grained gabbronorite veins is present centered at c. 72 cm and 83 cm."	"Almost completely serpentinized dunite and harzburgite; the latter is cut by two hydrothermally altered magmatic veins. The altered magmatic veins contain clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. The vein is cut by prehnite veins that grade to picrolite in the serpentinized peridotites. Mesh is green, brown, and grey. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive magnetite veins, and massive picrolite veins. The latter cut through the magmatic veins."	"Strongly foliated dunite with moderate mesh foliation (subhorizontal), above serpentinized harzburgite. Isotropic undeformed gabbro intrudes at harzburgite-dunite contact. Local magnetite veins in dunite. Harzburgite is locally protomylonitic at gabbro contact."	
"399"	"U1601"	"C"	"80"	"R"	"1"	""	"399-U1601C-80R-1"	"0.0"	"122.5"	"401.300"	"401.913"	"402.525"	"401.3"	"401.851"	"402.402"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Mostly harzburgite, but with a chromium-spinel-bearing dunite from 96.5 10 100 cm. Most orthopyroxene in the harzburgite is of the granular variety. The boundary between the dunite and harzburgite has orthopyroxene trails."	"Variably serpentinized harzburgite and minor dunite; the latter is completely serpentinized. Spinel is fresh. In the dunite-rich zones, the spinel turns brown. The mesh is black to green. Pieces #1, and 2 show green color. The last four pieces are less serpentinized than the others. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Serpentinized harzburgite with protogranular to strong foliation. Regular mesh in protogranular interval; incipient to no mesh in strongly foliated interval with dunite horizons with gentle dip. Little white veins follow foliation, but are anastomosing around OPX grains."	
"399"	"U1601"	"C"	"80"	"R"	"2"	""	"399-U1601C-80R-2"	"0.0"	"143.0"	"402.525"	"403.240"	"403.955"	"402.406"	"403.052"	"403.698"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Most of the section is pyroxene-enriched harzburgite (up to 29% orthopyroxene and 1% clinopyroxene) with trace spinel. This harzburgite has 2-4 cm-sized pyroxene clusters and olivine wherlite veins centered at 5 and 53 cm."	"Variably serpentinized Cpx-bearing harzburgite cut by several types of veins including serpentine-magnetite, fibrous to massive chrysotile veins, and massive picrolite veins."	"Strongly foliated serpentinized harzburgite with large 4-5cm opx and incipient mesh; gently dipping little white veins anastomose around opx grains."	
"399"	"U1601"	"C"	"80"	"R"	"3"	""	"399-U1601C-80R-3"	"0.0"	"127.0"	"403.955"	"404.590"	"405.225"	"403.698"	"404.272"	"404.845"	""	"1, 2, 3"	""	"Most of the section is pyroxene-enriched harzburgite like that in the overlying section. The exception is a 1 mm gabbronorite vein centered at 39 cm."	"Variably serpentinized Cpx-bearing harzburgite cut by thin hydrothermally altered magmatic veins. The latter contain clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and picrolite veins. The magmatic vein is also cut by picrolite and chrysotile veins."	"Strongly foliated serpentinized harzburgite (10° dip) with anastomosing, incipient mesh, and poorly developed little white veins cut by a magmatic vein (moderate dip)."	
"399"	"U1601"	"C"	"80"	"R"	"4"	""	"399-U1601C-80R-4"	"0.0"	"150.0"	"405.225"	"405.975"	"406.725"	"404.845"	"405.522"	"406.2"	""	"1, 2, 3, 4, 5, 6"	""	"Most of the section is pyroxene-enriched harzburgite like that in the overlying section. The exception is a 8 mm gabbronorite vein centered at 84cm."	"Variably serpentinized Cpx-bearing harzburgite cut by thin hydrothermally altered magmatic veins containing clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and picrolite veins. The magmatic vein is also cut by picrolite veins."	"Strongly foliated to protogranular serpentinized harzburgite with incipient mesh; gently dipping little white veins anastomose around opx grains; shallow dip magmatic vein."	
"399"	"U1601"	"C"	"81"	"R"	"1"	""	"399-U1601C-81R-1"	"0.0"	"133.5"	"406.200"	"406.868"	"407.535"	"406.2"	"406.827"	"407.455"	""	"1, 2, 3, 4"	""	"Harzburgite with c. 25 % orthopyroxene both granular and interstitial orthopyroxene and trace clinopyroxene and spinel. A several-cm-thick highly altered gabbro vein is centered at c. 78 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein composed of amphibole, chlorite, secondary plagioclase, prehnite, and potentially epidote. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive composite picrolite-serpentine veins. The magmatic vein is crosscut by one chlorite vein."	"Weakly foliated serpentinized harzburgite (subhorizontal mantle fabric) with incipient mesh. Cut by moderat dip magmatic intrusion."	
"399"	"U1601"	"C"	"81"	"R"	"2"	""	"399-U1601C-81R-2"	"0.0"	"117.0"	"407.535"	"408.120"	"408.705"	"407.454"	"408.003"	"408.553"	""	"1, 2, 3"	""	"Harzburgite with c. 20 % orthopyroxene both granular and interstitial orthopyroxene and trace percent clinopyroxene and spinel. Two 1-2 mm wide gabbronorite veins are centered at 34 and 81 cm."	"Highly serpentinized harzburgite cut by four hydrothermally altered magmatic veins composed of clinopyroxene and plagioclase, as well as secondary amphibole, chlorite, plagioclase, and prehnite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic veins."	"Weakly foliated serpentinized harzburgite with subhorizontal moderately foliated mesh."	
"399"	"U1601"	"C"	"81"	"R"	"3"	""	"399-U1601C-81R-3"	"0.0"	"146.5"	"408.705"	"409.438"	"410.170"	"408.553"	"409.241"	"409.93"	""	"1, 2, 3, 4"	""	"Harzburgite with c. 20 % orthopyroxene both granular and interstitial orthopyroxene and trace clinopyroxene and spinel. Grain size of orthopyroxene is variable."	"Highly serpentinized harzburgite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive composite picrolite-chrysotile veins."	"Protogranular serpentinized harzburgite with weakly foliated mesh, cut by 40° dipping little white veins."	
"399"	"U1601"	"C"	"81"	"R"	"4"	""	"399-U1601C-81R-4"	"0.0"	"114.0"	"410.170"	"410.740"	"411.310"	"409.929"	"410.464"	"411"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with c. 20 % orthopyroxene both granular and interstitial orthopyroxene and trace clinopyroxene and spinel. Grain size of orthopyroxene is variable. A 3-cm-wide olivine gabbronorite vein cuts the harzburgite in the top 31 cm. The contact between the domains is sutured."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. The latter is made of clinopyroxene, plagioclase, secondary amphibole, chlorite, plagioclase, and prehnite. It is cut by prehnite-carbonate veins and chlorite veins. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and massive composite picrolite-chrysotile veins. The latter also cuts through the magmatic vein."	"Protogranular serpentinized harzburgite with moderately foliated subhorizontal mesh; cut by horizontal and 25° dipping little white veins, and subvertical and moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"82"	"R"	"1"	""	"399-U1601C-82R-1"	"0.0"	"142.0"	"411.000"	"411.710"	"412.420"	"411"	"411.71"	"412.42"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with c. 20 % orthopyroxene both granular and interstitial orthopyroxene and a trace clinopyroxene. Orthopyroxene size and abundance decreases toward gabbro domain. The gabbro domain is between 96.5 and 117 cm. It is coarse grained, with swept-in olivine along its boundary with the harzburgite."	"Highly serpentinized harzburgite and Opx-bearing to Opx-free dunite at the contact with altered gabbro. Gabbro is composed of clinopyroxene, plagioclase, secondary amphibole, chlorite, plagioclase, and prehnite. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and massive chrysotile veins."	"Protogranular to weakly foliated serpentinized harzburgite with gabbro interval. Cut by thick, gently dipping magnetite veins."	
"399"	"U1601"	"C"	"82"	"R"	"2"	""	"399-U1601C-82R-2"	"0.0"	"134.5"	"412.420"	"413.092"	"413.765"	"412.42"	"413.092"	"413.765"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with c. 22 % orthopyroxene and a trace clinopyroxene. Cm-scale olivine websterite clusters are present. Some of these clusters also have chromium spinel. A coarse-grained gabbro vein cuts the harzburgite between 115.5 and 118.5 cm."	"Highly serpentinized harzburgite and Opx-bearing to Opx-free dunite. The dunite is cut by a hydrothermally altered magmatic vein composed of clinopyroxene, secondary amphibole, chlorite, plagioclase, prehnite, and sulfides. It is crosscut by prehnite veins and chlorite veins. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive chrysotile-carbonate veins."	"Protogranular serpentinized harzburgite with subhorizontal weak mesh. Gabbro interval with subhorizontal contact. Two orientations of little white veins dipping 0 and 25°. "	
"399"	"U1601"	"C"	"82"	"R"	"3"	""	"399-U1601C-82R-3"	"0.0"	"106.0"	"413.765"	"414.295"	"414.825"	"413.765"	"414.295"	"414.825"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Harzburgite with c. 22 % orthopyroxene and a trace clinopyroxene down to 15 cm, with a coarse grained norite(?) below. Beneath the norite is an orthopyroxene-bearing dunite to 49 cm. A harzburgite with trace clinopyroxene composes the rest of the section."	"Highly serpentinized Opx-bearing dunite and altered gabbro. Dunite is cut by a hydrothermally altered magmatic vein. Gabbro is made of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. The hydrothermally altered magmatic vein is made of plagioclase, amphibole, chlorite, and secondary plagioclase. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile, massive picrolite, and composite chrysotile-carbonate veins. The massive picrolite veins also cut through the magmatic vein."	"Protogranular serpentinized harzburgite with gabbro interval."	
"399"	"U1601"	"C"	"82"	"R"	"4"	""	"399-U1601C-82R-4"	"0.0"	"90.5"	"414.825"	"415.277"	"415.730"	"414.825"	"415.277"	"415.73"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with c. 2 % orthopyroxene and a trace clinopyroxene. Cut by a 2 mm wide gabbronorite vein centered at 72 cm."	"Highly serpentinized Opx-bearing dunite cut by a hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase and amphibole, chlorite, secondary plagioclase, and prehnite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by steeply dipping magmatic veins"	
"399"	"U1601"	"C"	"83"	"R"	"1"	""	"399-U1601C-83R-1"	"0.0"	"144.0"	"415.900"	"416.620"	"417.340"	"415.9"	"416.62"	"417.34"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Harzburgite with c. 15 % orthopyroxene and a trace clinopyroxene. Cut by gabbro with remarkably acicular clinopyroxene from 30 to 46 cm."	"Highly serpentinized harzburgite, dunite, and altered gabbro. Harzburgite is cut by two hydrothermally altered magmatic veins. Gabbro is composed of amphibole, chlorite, secondary plagioclase, and prehnite. It is crosscut by chlorite and zeolite veins. Magmatic veins in serpentinite are made of plagioclase and chlorite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive chrysotile and picrolite veins. Picrolite veins also cut through the magmatic veins."	"Protogranular serpentinized harzburgite with regular to weakly foliated subhorizontal mesh, cut by isotropic pegmatitic gabbro interval, and various orientations of little white veins. "	
"399"	"U1601"	"C"	"83"	"R"	"2"	""	"399-U1601C-83R-2"	"0.0"	"136.0"	"417.340"	"418.020"	"418.700"	"417.34"	"418.02"	"418.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Harzburgite with c. 17 % orthopyroxene and a trace clinopyroxene. Has domains of coarse-grained olivine-bearing gabbro that splays with a finer grain size into the harzburgite with contacts that are sutured and irregular."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veins. Highly altered gabbro. The latter is made of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. It is crosscut by carbonate, chlorite, and prehnite veins. Magmatic veins are made of plagioclase, amphibole, prehnite, and chlorite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive chrysotile and picrolite veins. Picrolite veins also cut through the magmatic veins."	"Protogranular serpentinized harzburgite with regular to no mesh. Gabbro interval isotropic with a steep contact against harzburgite.  Cut by white and green veins."	
"399"	"U1601"	"C"	"83"	"R"	"3"	""	"399-U1601C-83R-3"	"0.0"	"110.5"	"418.700"	"419.252"	"419.805"	"418.7"	"419.252"	"419.805"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with c. 17 % orthopyroxene and trace clinopyroxene."	"Highly serpentinized harzburgite. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by little white veins of various orientation."	
"399"	"U1601"	"C"	"83"	"R"	"4"	""	"399-U1601C-83R-4"	"0.0"	"61.5"	"419.805"	"420.113"	"420.420"	"419.805"	"420.113"	"420.42"	""	"1, 2, 3, 4"	""	"Harzburgite with c. 17 % orthopyroxene and trace clinopyroxene."	"Highly serpentinized harzburgite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile veins, and late massive picrolite veins."	"Protogranular serpentinized harzburgite with weakly foliated (subhorizontal) to regular mesh, cut by little white veins."	
"399"	"U1601"	"C"	"84"	"R"	"1"	""	"399-U1601C-84R-1"	"0.0"	"130.0"	"420.700"	"421.350"	"422.000"	"420.7"	"421.35"	"422"	""	"1, 2, 3, 4, 5, 6"	""	"The top 6 cm is orthopyroxene-bearing dunite. It is underlain by harzburgite with c. 18 % orthopyroxene and trace clinopyroxene. Cpx proportion increases down section. Has a 4 mm wide diffuse vein of alteration minerals, likely after gabbro centered at 36 cm."	"Highly serpentinized harzburgite. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by steeply dipping magmatic vein. "	
"399"	"U1601"	"C"	"84"	"R"	"2"	""	"399-U1601C-84R-2"	"0.0"	"108.0"	"422.000"	"422.540"	"423.080"	"422"	"422.54"	"423.08"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with c. 18 % orthopyroxene and trace clinopyroxene.  Has two mm-scale veins of gabbronorite centered at 61 and 88 cm. "	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veins. The latter is made of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile veins cutting through a fibrous chrysotile network, and picrolite veins. The picrolite veins also cut the magmatic veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by steeply dipping magmatic vein. "	
"399"	"U1601"	"C"	"84"	"R"	"3"	""	"399-U1601C-84R-3"	"0.0"	"128.5"	"423.080"	"423.723"	"424.365"	"423.08"	"423.723"	"424.365"	""	"1, 2, 3, 4"	""	"Harzburgite with c.  % orthopyroxene and 1% clinopyroxene."	"Highly serpentinized harzburgite cut by two small hydrothermally altered magmatic veins composed of chlorite, secondary plagioclase, and amphibole. The serpentinized peridotite is cut by serpentine-magnetite and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by moderately dipping magmatic vein.  "	
"399"	"U1601"	"C"	"84"	"R"	"4"	""	"399-U1601C-84R-4"	"0.0"	"80.5"	"424.365"	"424.767"	"425.170"	"424.365"	"424.767"	"425.17"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with c. 19 % orthopyroxene and clinopyroxene decreasing down section from 1 to 0 %.  "	"Highly serpentinized harzburgite cut by one small hydrothermally altered magmatic vein composed of amphibole, secondary plagioclase, and chlorite. White and green bastite after clinopyroxene (?) and orthopyroxene, respectively. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, thick fibrous chrysotile veins that cut through the network of fibrous chrysotile veins, and massive picrolite veins cutting through all the aforementioned veins. The picrolite veins also cut through the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh, cut by steeply dipping gran veins."	
"399"	"U1601"	"C"	"85"	"R"	"1"	""	"399-U1601C-85R-1"	"0.0"	"122.0"	"425.600"	"426.210"	"426.820"	"425.6"	"426.165"	"426.73"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Pyroxene-rich harzburgite (28% orthopyroxene, 1% clinopyroxene). Has few-mm scale gabbronorite veins centered at 41 cm, 61, and 89 cm."	"Highly to completely serpentinized harzburgite cut by two hydrothermally altered magmatic veins composed of amphibole and a pink-brown mineral after clinopyroxene, chlorite, secondary plagioclase, and possibly epidote. White bastite possibly composed of serpentine after possibly clinopyroxene. Green bastite after orthopyroxene, is made of serpentine and talc. The serpentinized peridotite is cut by several types of veins including mesh, a network of fibrous to massive chrysotile veins, chrysotile-oxide veins, and slickensides of chrysotile along fractures that cut all the aforementioned veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by moderately dipping magmatic vein.  "	
"399"	"U1601"	"C"	"85"	"R"	"2"	""	"399-U1601C-85R-2"	"0.0"	"133.0"	"426.820"	"427.485"	"428.150"	"426.73"	"427.346"	"427.963"	""	"1, 2, 3, 4, 5, 6"	""	"Pyroxene-rich harzburgite (25% orthopyroxene, 2% clinopyroxene)."	"Highly to completely serpentinized harzburgite. White bastite possibly composed of serpentine after clinopyroxene (?). Green bastite after orthopyroxene made of serpentine. The serpentinized peridotite is cut by several types of veins including serpentine-magnetite veins, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with no mesh, cut by little white veins."	
"399"	"U1601"	"C"	"85"	"R"	"3"	""	"399-U1601C-85R-3"	"0.0"	"146.0"	"428.150"	"428.880"	"429.610"	"427.963"	"428.639"	"429.316"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Pyroxene-rich harzburgite (25% orthopyroxene, 3% clinopyroxene). Has mm to cm scale granular gabbronorite veins centered at 50 cm, 86, 110, 128 and 141 cm."	"Highly to completely serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of chlorite, amphibole, and a pink-brown mineral after clinopyroxene, as well as secondary plagioclase. Fresh spinel. White bastite is possibly composed of serpentine and talc after clinopyroxene (?). Green bastite after orthopyroxene is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with no mesh, cut by a fualt and little white veins. "	
"399"	"U1601"	"C"	"85"	"R"	"4"	""	"399-U1601C-85R-4"	"0.0"	"117.0"	"429.610"	"430.195"	"430.780"	"429.316"	"429.858"	"430.4"	""	"1, 2, 3, 4"	""	"Harzburgite with c. 20 % orthopyroxene, 1% clinopyroxene, and trace chromium spinel.  "	"Highly to completely serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of secondary plagioclase and chlorite. White bastite is composed of serpentine after clinopyroxene (?). Green bastite after orthopyroxene is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, a network of fibrous to massive chrysotile veins, massive chrysotile veins that cut through the chrysotile network, and massive picrolite veins."	"Protogranular serpentinized harzburgite with no mesh. Cut by moderate dip magmatic veins, cut by a reverse sense fault, and little white veins."	
"399"	"U1601"	"C"	"86"	"R"	"1"	""	"399-U1601C-86R-1"	"0.0"	"140.0"	"430.400"	"431.100"	"431.800"	"430.4"	"431.1"	"431.8"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with c. 20 % orthopyroxene and trace clinopyroxene and chromium spinel.  "	"Highly to completely serpentinized harzburgite cut by diffuse hydrothermally altered magmatic veins composed of secondary plagioclase and chlorite. White bastite is composed of serpentine after clinopyroxene (?). Green bastite after orthopyroxene is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite, a network of fibrous to massive chrysotile veins, massive chrysotile veins, and massive picrolite veins. The picrolite veins cut through the magmatic veins."	"Protogranular to porphyroclastic (with 35° dipping mantle fabric) serpentinized harzburgite, with no mesh to weakly foliated mesh (35° dip), cut by moderate to steeply dipping green veins."	
"399"	"U1601"	"C"	"86"	"R"	"2"	""	"399-U1601C-86R-2"	"0.0"	"140.0"	"431.800"	"432.500"	"433.200"	"431.8"	"432.5"	"433.2"	""	"1"	""	"Harzburgite containing relatively high fresh olivine. It averages 18% orthopyroxene and trace clinopyroxene and spinel. The orthopyroxene proportion decreases towards the end of the section. Contains one granular gabbronorite vein 5 mm in width centered at 41 cm."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, secondary plagioclase, chlorite, prehnite, and amphibole. White bastite is possibly composed of serpentine after clinopyroxene (?). Green bastite after orthopyroxene is made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The picrolite veins cut through the magmatic veins."	"Porphyroclastic (15° dip) serpentinized harzburgite with regular to no mesh, cut by late veins (magmatic (steep dip) and picrolite veins that eliminates  mesh in the associated alteration halo."	
"399"	"U1601"	"C"	"86"	"R"	"3"	""	"399-U1601C-86R-3"	"0.0"	"114.0"	"433.200"	"433.770"	"434.340"	"433.2"	"433.77"	"434.34"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"The top 8.5 cm is orthopyroxene-bearing dunite with trace chromium spinel. it is underlain by 2 cm of medium-grained granular gabbronorite. The rest of the section is relatively orthopyroxene poor harzburgite, except for an exotic gabbronorite pebble at 19-22 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins, as well as altered gabbro (one piece, 19-22 cm) made of clinopyroxene, plagioclase, secondary plagioclase, zeolite. The magmatic vein is made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Green to black bastite after orthopyroxene made of serpentine. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile veins, and  picrolite veins. The picrolite veins cut through the magmatic veins."	"Protogranular dark green-black serpentinized harzburgite and dunite interval with subhorizontal weakly foliated mesh. Small gabbroic interval has microfaults."	
"399"	"U1601"	"C"	"86"	"R"	"4"	""	"399-U1601C-86R-4"	"0.0"	"85.0"	"434.340"	"434.765"	"435.190"	"434.34"	"434.765"	"435.19"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 15% orthopyroxene."	"Highly serpentinized harzburgite. Bastite changes in color from grey to black; the latter has a brown corona. Mesh looks yellowish brown. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins, and small sulfides veinlets locally forming a network."	"Protogranular dark green-black serpentinized harzburgite with no mesh."	
"399"	"U1601"	"C"	"87"	"R"	"1"	""	"399-U1601C-87R-1"	"0.0"	"150.0"	"435.300"	"436.050"	"436.800"	"435.3"	"436.05"	"436.8"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26"	""	"Harzburgite with 15% orthopyroxene and trace chromium spinel. Few-mm-scale gabbronorite veins are centered at c. 13.5 cm and 30 cm. A highly altered, coarse grained gabbro intrudes between 49.5 and 78 cm. It is associated sulfide-bearing alteration veins."	"Highly serpentinized harzburgite and Opx-bearing dunite. The harzburgite is cut by hydrothermally overprinted magmatic veins. The magmatic veins are made of clinopyroxene, amphibole, chlorite, secondary plagioclase, and possibly prehnite. Highly altered gabbro is made of amphibole, chlorite, secondary plagioclase, and zeolite. Bastite is mainly grey. The serpentinized peridotite is cut by several types of veins including serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins, and small sulfides veins along fractures."	"Protogranular dark green-black serpentinized harzburgite with no mesh,  cut by gabbro with moderate dip."	
"399"	"U1601"	"C"	"87"	"R"	"2"	""	"399-U1601C-87R-2"	"0.0"	"126.0"	"436.800"	"437.430"	"438.060"	"436.8"	"437.43"	"438.06"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Harzburgite with minimal orthopyroxene, no clinopyroxene, and and trace chromium spinel. Has many bands and veins of medium-grained and highly-altered gabbro. Some alteration veins associated with the gabbro have sulfides. Olivine is present in the gabbro at 188 cm."	"Highly serpentinized harzburgite cut by a set of hydrothermally altered magmatic veins. The magmatic veins are made of amphibole, chlorite, secondary plagioclase, and prehnite. Mineralogical proportions vary from vein to vein. Highly altered and bleached gabbro made of amphibole after clinopyroxene, chlorite, secondary plagioclase, and possibly epidote after plagioclase. It is cut by zeolite veins. Bastite is mainly grey. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins, and prehnite-carbonate-chlorite/serpentine-sulfides veins. Picrolite and prehnite-carbonate-chlorite/serpentine-sulfides veins cut also through the magmatic veins."	"Protogranular dark green-black serpentinized harzburgite with no mesh. Cut by gabbro with cataclastic overprint. High density of veins cut harzburgite and gabbro, including calcite-sulfide veins."	
"399"	"U1601"	"C"	"87"	"R"	"3"	""	"399-U1601C-87R-3"	"0.0"	"86.0"	"438.060"	"438.490"	"438.920"	"438.06"	"438.49"	"438.92"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with minimal orthopyroxene and no clinopyroxene, but with trace chromium spinel. Crosscut by intrusions of medium- to coarse-grained and altered gabbro. The most prominent intrusions are centered at 10 and 82 cm. Some alteration veins associated with the gabbro have sulfides. "	"Highly serpentinized harzburgite cut by a set of hydrothermally altered magmatic veins. The magmatic veins are made of amphibole, chlorite, secondary plagioclase, prehnite, and possibly zeolite. Mineralogical proportions vary from vein to vein. Two intervals of gabbro with different extents of alteration and bleaching; one at the top (0-13 cm) and one at the bottom (77-86 cm). Gabbro at the top is black and white and made of possibly primary amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Highly altered and bleached gabbro at the bottom of the section made of amphibole after clinopyroxene, chlorite, secondary plagioclase, and possibly epidote after plagioclase. It is crosscut by carbonate veins that grade to picrolite when propagating in the harzburgite. Bastite is mainly grey. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins that locally connect with carbonate-sulfide veins, massive picrolite veins, and prehnite-carbonate-chlorite-sulfides veins. Picrolite and prehnite-carbonate-chlorite-sulfides veins cut also through the magmatic veins."	"Protogranular dark green-black serpentinized harzburgite with no mesh. Cut by brecciated/fractured gabbro with a steep dip. High density of veins cutting harzburgite and gabbro."	
"399"	"U1601"	"C"	"87"	"R"	"4"	""	"399-U1601C-87R-4"	"12.0"	"102.0"	"439.040"	"439.490"	"439.940"	"439.04"	"439.49"	"439.94"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with minimal orthopyroxene, no clinopyroxene., and trace chromium spinel. Crosscut by exceedingly altered gabbroic  intrusions focused in the upper 30 cm, with scattered veins below. Some veins have sulfides. "	"Highly serpentinized Opx-bearing dunite and harzburgite cut by three hydrothermally altered magmatic veins. The magmatic veins are made of amphibole after clinopyroxene, chlorite, secondary plagioclase, prehnite, and possibly zeolite. Mineralogical proportions vary from vein to vein. Highly altered and bleached gabbro at the top of the section made of amphibole after clinopyroxene, chlorite, and an unknown white mineral. It is crosscut by zeolite veins. Bastite is mostly black and locally grey. At the contact between magmatic veins and peridotite, sulfide mineralization occurs. The serpentinized peridotite is cut by several types of veins including mesh, network of fibrous to massive chrysotile veins, massive picrolite veins, and composite carbonate-chlorite/serpentine-sulfides veins. Picrolite and carbonate-chlorite-serpentine-sulfides veins cut also through the magmatic veins."	"Serpentinized harzburgite with brecciated/fractured gabbro interval, cut by thick 4cm white fibrous vein, and late white veins."	
"399"	"U1601"	"C"	"88"	"R"	"1"	""	"399-U1601C-88R-1"	"0.0"	"150.0"	"440.100"	"440.850"	"441.600"	"440.1"	"440.85"	"441.6"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"Harzburgite with 12% orthopyroxene and trace clinopyroxene. Granular and interstitial orthopyroxene is evident. The harzburgite is cut by altered medium grained and altered gabbro at several levels in the section. The most prominent of intrusion is centered at 55 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, chlorite, and secondary plagioclase. Highly altered gabbro (1-6 and 48-61 cm) made of amphibole after clinopyroxene, chlorite, secondary plagioclase, and prehnite. It is cut by chlorite and zeolite veins. Bastite is black in the dunite between the two gabbro layers and grey in the harzburgite down section. The serpentinized peridotite is cut by several types of veins including mesh, network of fibrous to massive chrysotile veins, massive picrolite veins, sulfides veins, and carbonate-sulfides veins. Picrolite also cut through the magmatic veins."	"Protogranular serpentinized harzburgite with no  to weakly foliated (horizontal) mesh. Gabbro interval, cut by magmatic veins cut by green veins."	
"399"	"U1601"	"C"	"88"	"R"	"2"	""	"399-U1601C-88R-2"	"0.0"	"136.0"	"441.600"	"442.280"	"442.960"	"441.6"	"442.28"	"442.96"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with 12% orthopyroxene down to 130 cm. Granular and interstitial orthopyroxene is evident. Clinopyroxene forms linear trails together with chromium spinel.  The rest of the section consists of a pebble of orthopyroxene-bearing dunite and a cobble of altered gabbro."	"Highly serpentinized harzburgite and Opx-bearing dunite. A pebble of hydrothermally altered gabbro at the bottom of the section consists of amphibole, chlorite, secondary plagioclase. It is cut by a white vein of unknown mineral. Bastite is mostly black with a brown corona to grey. White bastite could have been formed after clinopyroxene. The serpentinized peridotite is cut by serpentine-magnetite veins, network of fibrous to massive chrysotile veins, and one massive picrolite-magnetite vein."	"Protogranular serpentinized harzburgite with no to regular mesh. Cut by green black veins. Section hosts very prominent strings of altered pyroxene that do not follow grain boundaries, with moderate dip."	
"399"	"U1601"	"C"	"88"	"R"	"3"	""	"399-U1601C-88R-3"	"0.0"	"150.0"	"442.960"	"443.710"	"444.460"	"442.96"	"443.71"	"444.46"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"The top 33 cm is orthopyroxene-bearing dunite cut by coarse-grained olivine-bearing gabbro with a troctolitic contact. Harzburgite with a trace of clinopyroxene makes up the center of the section. The interval from 89.5 to 132 cm is dunite with trace chromium spinel. The base of the section is orthopyroxene-bearing olivine gabbro with a troctolitic reaction boundary against the dunite."	"Highly serpentinized harzburgite and Opx-bearing dunite. The dunite is cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Hydrothermally altered gabbro at the bottom of the section consisting of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. There is a prehnite-rich area at the contact between the gabbro and the serpentinite. The gabbro is cut by one chlorite vein. Spinel looks fresh. Bastite is mostly black to grey. A patchy area contains green mesh in Opx-bearing dunite. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, thicker massive chrysotile veins, massive picrolite veins, and carbonate-black mineral veins."	"Protogranular serpentinized harzburgite above dark to black dunite with steep contact against altered gabbro with a protomylonite fabric oblique to the contact."	
"399"	"U1601"	"C"	"89"	"R"	"1"	""	"399-U1601C-89R-1"	"0.0"	"144.0"	"445.000"	"445.720"	"446.440"	"445"	"445.704"	"446.408"	""	"1, 2, 3, 4"	""	"Gabbro and harzburgite pebbles at the top, likely accidental. The rest is a standard harzburgite with 20% orthopyroxene (granular and interstitial) and a trace of clinopyroxene."	"Highly serpentinized harzburgite. One pebble of hydrothermally altered Ol-bearing gabbro at the top of the section consists of serpentine and magnetite after olivine, plagioclase, amphibole, chlorite, and secondary plagioclase. It is cut by one chlorite vein. Spinel looks fresh. Bastite is mostly green with a greenish-brown rim. The serpentinized peridotite is cut by serpentine-magnetite, fibrous to massive chrysotile veins, and one thicker stepped chrysotile vein."	"Protogranular to weakly foliated (20° dip) serpentinized harzburgite with localized patchy mesh below isotropic gabbro."	
"399"	"U1601"	"C"	"89"	"R"	"2"	""	"399-U1601C-89R-2"	"0.0"	"144.0"	"446.440"	"447.160"	"447.880"	"446.408"	"447.111"	"447.815"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Mostly standard harzburgite with 20% orthopyroxene (granular and interstitial) and a trace of clinopyroxene. Has a 1 mm gabbronorite vein centered at 85 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein. The latter is made of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. Bastite is mostly green with a greenish-brown rim. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. Picrolite veins cut also through the magmatic vein"	"Protogranular to weakly foliated (25° dip) serpentinized harzburgite with no mesh to regular mesh."	
"399"	"U1601"	"C"	"89"	"R"	"3"	""	"399-U1601C-89R-3"	"0.0"	"103.0"	"447.880"	"448.395"	"448.910"	"447.815"	"448.318"	"448.822"	""	"1, 2, 3, 4, 5"	""	"Mostly standard harzburgite with 18% orthopyroxene (granular and interstitial) and a trace of clinopyroxene. Has three mm-scale gabbronorite veins centered at 31, 58, and 73 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein containing clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. Bastite is mostly green with a greenish-brown rim. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. Picrolite veins cut also through the magmatic vein"	"Protogranular to weakly foliated (35° dip) serpentinized harzburgite with patchy regular mesh, cut by moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"89"	"R"	"4"	""	"399-U1601C-89R-4"	"0.0"	"100.0"	"448.910"	"449.410"	"449.910"	"448.822"	"449.311"	"449.8"	""	"1, 2, 3, 4, 5"	""	"Mostly standard harzburgite with 18% orthopyroxene (granular and interstitial) and a trace of clinopyroxene."	"Highly serpentinized harzburgite. Spinel looks fresh. Bastite is mostly green to grey with a greenish-brown rim. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular to weakly foliated (15deg) serpentinized harzburgite with incipient to patchy regular mesh. "	
"399"	"U1601"	"C"	"90"	"R"	"1"	""	"399-U1601C-90R-1"	"0.0"	"120.0"	"449.800"	"450.400"	"451.000"	"449.8"	"450.4"	"451"	""	"1, 2"	""	"Harzburgite with elevated orthopyroxene content (c. 20%) and trace chrome spinel and clinopyroxene."	"Highly serpentinized harzburgite. Spinel looks fresh. Bastite is mostly green to grey with greenish-brown rim. Chrysotile wraps the orthopyroxene bastite and olivine rims, forming an augen texture. Some of the mesh centers appear white but are completely serpentinized. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Partially serpentinized harzburgite with weak subhorizontal porphyroclastic mantle fabric and a regular mesh, cut by little white veins anastomose around pyroxene grains."	
"399"	"U1601"	"C"	"90"	"R"	"2"	""	"399-U1601C-90R-2"	"0.0"	"97.0"	"451.000"	"451.485"	"451.970"	"451"	"451.485"	"451.97"	""	"1, 2"	""	"Harzburgite with elevated orthopyroxene content (c. 20%) and trace chrome spinel and clinopyroxene."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein. The latter is made of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. Bastite is mostly green to grey with greenish-brown rim. Chrysotile wraps the orthopyroxene bastite and olivine rims, forming augen texture. Some of the mesh centers appear white but are completely serpentinized. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. Chrysotile veins cut the magmatic vein."	"Partially serpentinized harzburgite with weak subhorizontal porphyroclastic mantle fabric and regular mesh, cut by a moderate dipping magmatic veins."	
"399"	"U1601"	"C"	"90"	"R"	"3"	""	"399-U1601C-90R-3"	"0.0"	"133.0"	"451.970"	"452.635"	"453.300"	"451.97"	"452.635"	"453.3"	""	"1, 2"	""	"Harzburgite with elevated orthopyroxene content (c. 20%) and trace chrome spinel and clinopyroxene. Has two mm-scale gabbronorite veins centered at 70 and 91 cm."	"Moderately to highly serpentinized harzburgite cut by two hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Spinel looks fresh. Bastite is mostly green to grey with a greenish-brown rim. Chrysotile wraps the orthopyroxene bastite and olivine rims, forming an augen texture. Some of the mesh centers appear white but are completely serpentinized. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. Picrolite and chrysotile veins cut the magmatic vein."	"Partially serpentinized harzburgite with weak subhorizontal porphyroclastic mantle fabric and regular mesh, cut by a moderate dipping magmatic veins, and green veins."	
"399"	"U1601"	"C"	"90"	"R"	"4"	""	"399-U1601C-90R-4"	"0.0"	"110.0"	"453.300"	"453.850"	"454.400"	"453.3"	"453.85"	"454.4"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 25% orthopyroxene and trace chrome spinel and clinopyroxene. Has a 3-mm wide gabbronorite vein centered at 64 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase, chlorite, secondary plagioclase, and prehnite. Bastite is mostly green to grey. Small white bastite, possibly forming after clinopyroxene. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. Picrolite veins cut the magmatic vein."	"Protogranular to weak subhorizontal porphyroclastic serpentinized harzurgite, with weak foliated mesh cut by moderately dipping magmatic vein."	
"399"	"U1601"	"C"	"91"	"R"	"1"	""	"399-U1601C-91R-1"	"0.0"	"145.0"	"454.700"	"455.425"	"456.150"	"454.7"	"455.425"	"456.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"The top 28.5 cm is a course grained granular gabbro with a reactive troctolitic contact with the harzburgite. A harzburgite with 18% orthopyroxene and trace chromium spinel concludes the section. "	"Highly serpentinized harzburgite and hydrothermally altered gabbro composed of clinopyroxene, plagioclase, amphibole after clinopyroxene, chlorite, prehnite, and secondary plagioclase after plagioclase. Towards the serpentinized harzburgite, there is partly serpentinized olivine in the gabbro. The gabbro is cut by prehnite-chlorite and amphibole veins. Bastite is black with a brown rim close to the gabbro and turns green down-section. Mesh is brown close to the gabbro and features sulfides mineralization. Spinel looks fresh but shows a yellow metallic luster (sulfides?). Chrysotile network more pronounced downsection. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and locally composite carbonate-serpentine veins."	"Pegmatitic gabbro above protogranular serpentinized harzurgite, with no mesh, across gently dipping contact. "	
"399"	"U1601"	"C"	"91"	"R"	"2"	""	"399-U1601C-91R-2"	"0.0"	"141.0"	"456.150"	"456.855"	"457.560"	"456.15"	"456.855"	"457.56"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Harzburgite with 18% orthopyroxene and trace chromium spinel . "	"Highly serpentinized harzburgite. Bastite is green. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and late composite bronze mineral-chrysotile veins."	"Protogranular serpentinized harzburgite with no mesh."	
"399"	"U1601"	"C"	"91"	"R"	"3"	""	"399-U1601C-91R-3"	"0.0"	"85.0"	"457.560"	"457.985"	"458.410"	"457.56"	"457.985"	"458.41"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with 18% orthopyroxene and trace chromium spinel . "	"Highly serpentinized harzburgite. Bastite is green. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile veins, and composite brown reddish mineral-picrolite veins."	"Protogranular serpentinized harzburgite with no mesh."	
"399"	"U1601"	"C"	"92"	"R"	"1"	""	"399-U1601C-92R-1"	"0.0"	"147.0"	"459.500"	"460.235"	"460.970"	"459.5"	"460.235"	"460.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Harzburgite with 15% orthopyroxene with granular and interstitial textures. Trace chromium spinel. From 10 to 29.5 cm is a coarse-grained gabbronorite intrusion."	"Highly serpentinized harzburgite and altered gabbro. Gabbro is made of amphibole, plagioclase, chlorite, secondary plagioclase, prehnite, and zeolite. Bastite is green and displays a white corona close to the gabbro interval. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive chrysotile veins, massive picrolite veins, a single magnetite vein, and a composite chrysotile-carbonate vein."	"Protogranular serpentinized harzburgite with weak horizontal mesh, cut by isotropic gabbro, shallow contacts."	
"399"	"U1601"	"C"	"92"	"R"	"2"	""	"399-U1601C-92R-2"	"0.0"	"145.0"	"460.970"	"461.695"	"462.420"	"460.97"	"461.695"	"462.42"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"The top is domains of orthopyroxene-bearing dunite and highly altered gabbro with obscured original mineralogy and textures. From 86.5 to the base of the section is a medium grained olivine bearing gabbro with olivine near boundary with host peridotite. Grain size very variable on 10 cm scale. Highly deformed and altered. Contact at bottom sutured irregular intrusive boundary."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of clinopyroxene, chlorite, secondary plagioclase, prehnite, and a pinkish brown mineral (soft, possibly mixture of clays and zeolite). Highly altered gabbro (4-23 and 87-145 cm). Gabbro is made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, chlorite, prehnite, and a pinkish-brown mineral (soft, possibly a mixture of clays and zeolite). The latter is more abundant in the upper gabbro. The gabbro is cut by chlorite, amphibole, and prehnite veins. Bastite is black. The mesh is brown and contains sulfide-magnetite veins. Spinel looks fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, composite carbonate-chrysotile-sulfides veins, picrolite-sulfides veins, prehnite-chlorite-clays-sulfide veins, and sulfides veinlets."	"Protogranular serpentinized harzburgite with protomylonitic gabbro intervals cut by cataclastic bands cut by white-green veins."	
"399"	"U1601"	"C"	"92"	"R"	"3"	""	"399-U1601C-92R-3"	"0.0"	"126.5"	"462.420"	"463.053"	"463.685"	"462.42"	"463.053"	"463.685"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Harzburgite with multiple highly altered gabbroic veins. The best preserved is a c. 4 cm coarse-grained gabbro vein centered at 104 cm. Orthopyroxene-beraring dunite is found near the veins."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, amphibole, chlorite, secondary plagioclase, prehnite, pinkish brown mineral (soft, possibly mixture of clays and zeolite), and sulfides. Bastite is grey. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite, picrolite-sulfides veins, and carbonate-sulfides veins."	"Protogranular serpentinized harzburgite with no mesh, cut by foliated and fractured gabbro intervals (with steep contacts), and several big green picrolite veins have massive sulphides."	
"399"	"U1601"	"C"	"93"	"R"	"1"	""	"399-U1601C-93R-1"	"0.0"	"150.0"	"464.400"	"465.150"	"465.900"	"464.4"	"465.15"	"465.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The section is very similar to 93R-3, with the most prominent gabbroic veins found at the top of the section, at 85 cm, and at 105cm, "	"Highly serpentinized harzburgite and dunite. Harzburgite is cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Bastite is grey. The extent of serpentinization is variable. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh, cut by moderately dipping gabbro intervals, and steep magmatic veins, all cut by shallow green veins."	
"399"	"U1601"	"C"	"94"	"R"	"1"	""	"399-U1601C-94R-1"	"0.0"	"112.0"	"469.200"	"469.760"	"470.320"	"469.2"	"469.76"	"470.32"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 15% orthopyroxene and trace chromium spinel. A c. 10 mm-wide gabbronorite vein cuts through the harzburgite along much of the length of the section."	"Highly and variably serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, prehnite. Bastite is grey to locally green. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut the magmatic veins."	"Porphyroclastic serpentinized harzburgite with no mesh. Cut by 1cm thick magmatic veins in turn cut by perpendicular green veins, which become little white veins away fom magmatic vein. "	
"399"	"U1601"	"C"	"94"	"R"	"2"	""	"399-U1601C-94R-2"	"0.0"	"135.5"	"470.320"	"470.998"	"471.675"	"470.32"	"470.998"	"471.675"	""	"1, 2, 3, 4"	""	"Harzburgite with 15% orthopyroxene and trace chromium spinel. A c. 10 mm-wide gabbronorite vein cuts through the harzburgite in the top 27 cm of the section."	"Highly and variably serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, prehnite. Bastite is grey to locally green. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut the magmatic veins."	"Porphyroclastic serpentinized harzburgite with no mesh to very poorly developed patchy mesh.  White, 1cm wide magmatic veins are cut by perpendicular green veins, which become little white veins further away fom magmatic vein. Cut by subhorizontal little white veins."	
"399"	"U1601"	"C"	"94"	"R"	"3"	""	"399-U1601C-94R-3"	"0.0"	"150.0"	"471.680"	"472.430"	"473.180"	"471.68"	"472.43"	"473.18"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Harzburgite with 15 % orthopyroxene, trace clinopyroxene, and trace chromium spinel. Clinopyroxene disappears down section. The central and lower parts of the section have several gabbro veins with variable grain sizes."	"Highly and variably serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of plagioclase, chlorite, secondary plagioclase, and prehnite. Highly altered gabbro. The latter is made of clinopyroxene, plagioclase, amphibole, chlorite, secondary plagioclase, prehnite. It is cut by chlorite and sulfide veins. Bastite is black between the two gabbro intervals. It is green to grey elsewhere. The mesh between the two gabbro intervals appears brown. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Serpentinized harzburgite with gabbro intervals (moderate contact dip), no mesh. Gabbro is very altered. Contacts are often irregular. Cut by magmatic veins and green veins."	
"399"	"U1601"	"C"	"95"	"R"	"1"	""	"399-U1601C-95R-1"	"0.0"	"138.0"	"474.100"	"474.790"	"475.480"	"474.1"	"474.699"	"475.298"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 18 % orthopyroxene and trace chromium spinel. Two mm-scale veins consisting of secondary minerals are found at 40 and 108 cm. A c. 2 m wide altered leucocratic gabbro vein is present centered at 34 cm."	"Highly serpentinized harzburgite with variable orthopyroxene abundance. Serpentinite is cut by hydrothermally altered magmatic veins made of amphibole, plagioclase, chlorite, secondary plagioclase, prehnite, and a brownish material (mineral or stain after plagioclase?). Bastite appears black top section and becomes green down-section. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive chrysotile and picrolite veins."	"Protogranular serpentinized harzburgite regular mesh, cut by gently dipping magmatic vein cut by picrolite veins (steeper) and white veins."	
"399"	"U1601"	"C"	"95"	"R"	"2"	""	"399-U1601C-95R-2"	"0.0"	"140.0"	"475.480"	"476.180"	"476.880"	"475.298"	"475.906"	"476.513"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with 18-20 % orthopyroxene and trace chromium spinel. The top 53 cm also has dunite with a gradational boundary towards the harzburgite. "	"Highly serpentinized harzburgite and dunite. Bastite is grey to green. Mesh in the dunite (16-42 cm) is greenish to brown. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Steeply dipping contact between serpentinized harzburgite and dunite with  weakly foliated mantle fabric (10° dip), in serpentinized harzburgite below.        "	
"399"	"U1601"	"C"	"95"	"R"	"3"	""	"399-U1601C-95R-3"	"0.0"	"138.0"	"476.880"	"477.570"	"478.260"	"476.513"	"477.112"	"477.711"	""	"1, 2, 3, 04, 05"	""	"Harzburgite with 20 % orthopyroxene and trace chromium spinel. The top 53 cm also has dunite with a gradational boundary towards the harzburgite. The top 13 cm has a vein of medium-grained gabbro."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, amphibole, chlorite, prehnite, and secondary plagioclase. Bastite color changes from grey to green to dark green with the red corona. The extent of serpentinization is variable, with most abundant relicts of primary silicates close to the magmatic vein. Spinel variably altered. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins. The magmatic vein is cut by chlorite, picrolite, and zeolite veins."	"Protogranular to porphyroclastic (40° dipping mantle fabric) serpentinized harzburgite with no mesh, cut by steeply dipping magmatic vein, andlittle white veins (25° dip)."	
"399"	"U1601"	"C"	"95"	"R"	"4"	""	"399-U1601C-95R-4"	"0.0"	"137.0"	"478.260"	"478.945"	"479.630"	"477.711"	"478.305"	"478.9"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with 15% orthopyroxene, trace clinopyroxene, and trace chromium spinel. "	"Highly serpentinized harzburgite. Bastite is mostly grey to green. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Protogranular serpentinized harzburgite with no mesh to regular mesh."	
"399"	"U1601"	"C"	"96"	"R"	"1"	""	"399-U1601C-96R-1"	"0.0"	"150.0"	"478.900"	"479.650"	"480.400"	"478.9"	"479.65"	"480.4"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The top of the section grades from orthopyroxene-bearing dunite with trace chromium spinel to harzburgite. Granular and interstitial orthopyroxene are evident in the harzburgite. Few mm-thick highly altered gabbroic veins are found at 94 and 109 cm. From 116.5 to 130 cm is a highly altered leucogabbro containing sulfides. Below to the base of the section is harzburgite with 1% clinopyroxene and trace spinel."	"Highly serpentinized harzburgite and dunite. The harzburgite is cut by hydrothermally altered magmatic veins. The altered magmatic vein is made of prehnite, chlorite, and amphibole. Hydrothermally altered and bleached gabbro made of prehnite, chlorite, clinopyroxene, amphibole, and secondary plagioclase. Bastite changes in color from green upsection to grey downsection. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Protogranular to porphyroclstic serpentinized harzburgite with no mesh, cut by white altered foliated gabbro interval with moderately dipping magmatic fabric, and variable dip, steepening little white veins."	
"399"	"U1601"	"C"	"96"	"R"	"2"	""	"399-U1601C-96R-2"	"0.0"	"138.5"	"480.400"	"481.092"	"481.785"	"480.4"	"481.092"	"481.785"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial."	"Highly serpentinized harzburgite. Bastite is grey to green. Mesh in some areas is greenish, but most of it is grey-black. Spinel is variably altered to chlorite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Protogranular serpentinized harzburgite with regular mesh, cut by variably oriented little white veins."	
"399"	"U1601"	"C"	"96"	"R"	"3"	""	"399-U1601C-96R-3"	"0.0"	"150.0"	"481.790"	"482.540"	"483.290"	"481.79"	"482.54"	"483.29"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial. From 0 - 35 cm some dunitic patches"	"Highly serpentinized Opx-bearing dunite. Bastite is grey to green. Mesh in some areas is greenish, but most of it is grey-black. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and one composite picrolite-chrysotile vein."	"Protogranular serpentinized harzburgite with regular mesh, cut by gently dipping (20°) little white veins."	
"399"	"U1601"	"C"	"97"	"R"	"1"	""	"399-U1601C-97R-1"	"6.0"	"119.0"	"483.860"	"484.425"	"484.990"	"483.857"	"484.389"	"484.921"	""	"2, 3, 4, 5, 6"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial. A nearly vertical medium-grained gabbro vein cuts the the entire section."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Bastite is grey to green. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins. The picrolite veins cut through the magmatic veins."	"Protogranular serpentinized harzburgite with no mesh, cut by section-long vertical magmatic vein with a curved shape,  cut by green veins cut by shallow white veins."	
"399"	"U1601"	"C"	"97"	"R"	"2"	""	"399-U1601C-97R-2"	"0.0"	"140.5"	"484.990"	"485.692"	"486.395"	"484.921"	"485.582"	"486.242"	""	"1, 2, 3"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial. A nearly vertical medium-grained gabbro vein continues through 19 cm. "	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Bastite is grey to green. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins. The picrolite and chrysotile veins cut through the magmatic veins."	"Porphyroclastic (25° dipping mantle fabric) serpentinized harzburgite with patchy regular mesh. Little white veins anastomose parallel to mantle fabric. Cut by a moderate and shallow magmatic veins."	
"399"	"U1601"	"C"	"97"	"R"	"3"	""	"399-U1601C-97R-3"	"0.0"	"122.0"	"486.395"	"487.005"	"487.615"	"486.245"	"486.82"	"487.394"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Bastite is grey to green. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins. Chrysotile veins cut the magmatic vein."	"Protogranular serpentinized harzburgite regular mesh, cut by a magmatic vein (moderate dip), green veins, and variably oriented little white veins"	
"399"	"U1601"	"C"	"97"	"R"	"4"	""	"399-U1601C-97R-4"	"0.0"	"128.0"	"487.615"	"488.255"	"488.895"	"487.394"	"487.997"	"488.6"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 20% orthopyroxene, 1% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of amphibole, chlorite, and prehnite. Bastite is grey to green. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Protogranular serpentinized harzburgite with patchy regular mesh, cut by a magmatic vein (moderate dip) cut by variable little white veins."	
"399"	"U1601"	"C"	"98"	"R"	"1"	""	"399-U1601C-98R-1"	"0.0"	"131.0"	"488.600"	"489.255"	"489.910"	"488.6"	"489.255"	"489.91"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 20% orthopyroxene, 0.5% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial. The harzburgite is cut by by a coarse-grained granular gabbro from 104 to 110 cm."	"Moderately to highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein composed of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. Bastite is grey to green. Some areas show patches of greenish mesh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick picrolite veins."	"Protogranular serpentinized harzburgite with no mesh to regular mesh, cut by gently dipping little white veins and one magmatic vein (moderate dip). Three piece end faults with slickenfibers."	
"399"	"U1601"	"C"	"98"	"R"	"2"	""	"399-U1601C-98R-2"	"0.0"	"140.0"	"489.910"	"490.610"	"491.310"	"489.91"	"490.61"	"491.31"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with 20% orthopyroxene, 0.5% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veinlets made of amphibole, chlorite, and prehnite. Three pebbles of altered gabbro are composed of clinopyroxene, amphibole, chlorite, secondary plagioclase, and prehnite. Bastite is grey to green. Light green bastite possibly formed after clinopyroxene. Spinel is fresh. Some greenish mesh areas in patches. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins,"	"Protogranular to porphyroclastic serpentinized harzburgite with no mesh to regular mesh, cut by a magmatic vein."	
"399"	"U1601"	"C"	"98"	"R"	"3"	""	"399-U1601C-98R-3"	"0.0"	"121.0"	"491.310"	"491.915"	"492.520"	"491.31"	"491.915"	"492.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with 20% orthopyroxene, 0.5% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial."	"Highly serpentinized harzburgite. Bastite is grey to green. White bastite possibly after clinopyroxene. Some greenish mesh areas in patches. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite veins, and composite chrysotile-sulfide veins."	"Protogranular serpentinized harzburgite with patchy regular mesh, cut by gently dipping little white veins and two green veins (moderately dipping)."	
"399"	"U1601"	"C"	"98"	"R"	"4"	""	"399-U1601C-98R-4"	"0.0"	"92.0"	"492.520"	"492.980"	"493.440"	"492.52"	"492.98"	"493.44"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 20% orthopyroxene, 0.5% clinopyroxene, and trace chromium spinel. Orthopyroxene is granular and interstitial. A coarse-grained gabbro cuts the harzburgite between 19.5 and 39 cm. The gabbro contains olivine along the contact with the harzburgite."	"Highly serpentinized harzburgite. Altered gabbro with partially serpentinized olivine xenocrysts. Gabbro is made of clinopyroxene, plagioclase, amphibole, chlorite, prehnite, and secondary plagioclase. It is cut by zeolite veins. Bastite is grey to green. White bastite possibly after clinopyroxene. Some greenish mesh occurs in patches. Spinel is fresh. Disseminated sulfides in some of the dark green mesh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and one massive picrolite vein."	"Protogranular serpentinized harzburgite with no mesh to regular mesh, with shallow to moderate dip contacts with isotropic gabbro."	
"399"	"U1601"	"C"	"99"	"R"	"1"	""	"399-U1601C-99R-1"	"0.0"	"68.0"	"493.500"	"493.840"	"494.180"	"493.5"	"493.84"	"494.18"	""	"1, 2"	""	"Harzburgite with 20% orthopyroxene and trace chromium spinel. "	"Highly serpentinized harzburgite. Bastite is green to grey. Greenish mesh occurs in patches. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with no mesh to moderately foliated mesh, cut by little white veins that steepen with depth."	
"399"	"U1601"	"C"	"99"	"R"	"2"	""	"399-U1601C-99R-2"	"0.0"	"135.0"	"494.180"	"494.855"	"495.530"	"494.18"	"494.855"	"495.53"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 20% orthopyroxene and trace chromium spinel. A medium to coarse grained gabbro bordered by troctolite is at the base of the section. "	"Highly serpentinized harzburgite. Altered gabbro (119-135 cm) made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, chlorite, and amphibole. Bastite is green to grey. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, massive picrolite, and white serpentine veins."	"Protogranular serpentinized harzburgite with regular mesh."	
"399"	"U1601"	"C"	"99"	"R"	"3"	""	"399-U1601C-99R-3"	"0.0"	"143.0"	"495.530"	"496.245"	"496.960"	"495.53"	"496.245"	"496.96"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Medium grained olivine gabbro intermingled with troctolite. Some clinopyroxene in the gabbro is poikilitic. Prominant troctolite patches within the host gabbro are found at 11 cm and 120-126 cm with mm wide fingers stretching into the adjacent gabbro. "	"Variably altered gabbro and Ol-gabbro made of primary clinopyroxene, plagioclase, olivine and secondary plagioclase, prehnite, chlorite, serpentine, sulfides, oxides, and amphibole.  Cut by amphibole, chlorite, talc, carbonate, and zeolite veins."	"Isotropic, undeformed gabbro, with modal and grain size layering (contacts ith moderate dip)."	
"399"	"U1601"	"C"	"99"	"R"	"4"	""	"399-U1601C-99R-4"	"0.0"	"111.0"	"496.960"	"497.515"	"498.070"	"496.96"	"497.515"	"498.07"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Subophitic olivine gabbro with small patches of troctolite  throughout the section."	"Variably altered gabbro and Ol-gabbro, locally forming greenstone. It is made of primary clinopyroxene, plagioclase, and olivine, as well as secondary plagioclase, prehnite, chlorite, serpentine, sulfides, oxides, and amphibole. Cut by amphibole, chlorite, talc, and carbonate veins."	"Isotropic, undeformed gabbro with grain size layering, variably altered to bright green colours. Cut by parallel set of moderate dip, green-white veins."	
"399"	"U1601"	"C"	"100"	"R"	"1"	""	"399-U1601C-100R-1"	"0.0"	"145.0"	"498.300"	"499.025"	"499.750"	"498.3"	"499.025"	"499.75"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"The top bin has an accidental harzburgite pebble. From 2.4 to 77  cm are gabbroic. The upper portion is poikilitic olivine gabbro. Gabbro towards the bottom contact with harzburgite becomes coarser overall, with a coarse-grained granular domain and a medium-grained poikilitic domain. The boundary with harzburgite is troctolitic."	"Highly altered gabbro and highly serpentinized harzburgite. The gabbro is made of primary clinopyroxene, plagioclase, and secondary plagioclase, prehnite, chlorite, and amphibole. Bastite is green to grey. Cut by amphibole, chlorite, talc, prehnite, and carbonate veins. Carbonate veins grade to chrysotile when propagating in the serpentinized harzburgite. The serpentinized harzburgite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive picrolite and chrysotile veins."	"Isotropic gabbro, variable grain size, above protogranular serpentinized harzburgite, cut by green white veins."	
"399"	"U1601"	"C"	"100"	"R"	"2"	""	"399-U1601C-100R-2"	"0.0"	"118.0"	"499.760"	"500.350"	"500.940"	"499.76"	"500.35"	"500.94"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with trace clinopyroxene overlying dunite. Coarse-grained gabbro with a troctolitic border is present beneath 98.5 cm."	"Highly serpentinized harzburgite and altered gabbro (99-118 cm). The gabbro is made of primary clinopyroxene, plagioclase, and secondary plagioclase, prehnite, chlorite, amphibole, and sulfides. Sulfides are close to the contact with the serpentine. Olivine xenocrysts in the gabbro are partially serpentinized. The gabbro is cut by talc and zeolite veins. Bastite is green to grey. Spinel is fresh. Some chrysotile slickensides at the edges of some pieces. The serpentinized harzburgite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive white serpentine veins."	"Protogranular serpentinized harzburgite with regular to weakly foliated mesh above dunite with weakly foliated mesh and isotropic gabbro with horizontal contact."	
"399"	"U1601"	"C"	"100"	"R"	"3"	""	"399-U1601C-100R-3"	"0.0"	"57.0"	"500.940"	"501.225"	"501.510"	"500.94"	"501.225"	"501.51"	""	"1, 2, 3, 4, 5, 6, 7"	""	"The top 12 cm is gabbro continued from the overlying section. The rest is harzburgite with minimal orthopyroxene and trace clinopyroxene."	"Highly serpentinized harzburgite and altered gabbro (0-12 cm). The gabbro is composed of clinopyroxene and plagioclase, in addition to secondary plagioclase, prehnite, chlorite, and amphibole. It is cut by amphibole-chlorite veins. Bastite is green to grey. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive picrolite veins."	"Protogranular serpentinized harzburgite, moderately foliated mesh, small gabbro interval above."	
"399"	"U1601"	"C"	"101"	"R"	"1"	""	"399-U1601C-101R-1"	"0.0"	"150.0"	"503.200"	"503.950"	"504.700"	"503.2"	"503.907"	"504.614"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with 20% orthopyroxene, trace clinopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic veinlet. The latter is made of clinopyroxene, prehnite, chlorite, and amphibole. Three pieces contain fibrous chrysotile slickensides. Bastite is green to grey. Light green bastite could have formed after clinopyroxene. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive white serpentine veins."	"Protogranular serpentinized harzburgite with regular mesh cut by shallowly dipping little white veins."	
"399"	"U1601"	"C"	"101"	"R"	"2"	""	"399-U1601C-101R-2"	"0.0"	"66.0"	"504.700"	"505.030"	"505.360"	"504.614"	"504.925"	"505.237"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 20% orthopyroxene, trace clinopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic veinlet. The latter is made of secondary plagioclase, clinopyroxene, prehnite, and chlorite. One discontinuous vein. 3 pieces contain fibrous chrysotile slickensides. Bastite is green to grey. Light green bastite could have formed after clinopyroxene. Spinel is fresh. Greenish mesh occurs in patches."	"Protogranular serpentinized harzburgite with regular to weakly foliated mesh cut by shallow to moderately dipping white veins."	
"399"	"U1601"	"C"	"101"	"R"	"3"	""	"399-U1601C-101R-3"	"0.0"	"94.0"	"505.360"	"505.830"	"506.300"	"505.237"	"505.68"	"506.123"	""	"1, 2"	""	"Harzburgite with 1% orthopyroxene, trace clinopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite. Greenish mesh. Basitite green to grey. Light green bastite could have formed after clinopyroxene. Spinel is fresh. Patchy alteration of mesh which is lighter colored (greenish) when compared with the darker mesh. Serpentine-magnetite veins, chrysotile, and chlorite-picrolite veins."	"Protogranular serpentinized harzburgite with regular to weakly foliated mesh cut by moderate to shallowly dipping white and green veins."	
"399"	"U1601"	"C"	"101"	"R"	"4"	""	"399-U1601C-101R-4"	"0.0"	"118.0"	"506.300"	"506.890"	"507.480"	"506.123"	"506.68"	"507.236"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 20% orthopyroxene, trace clinopyroxene and trace chromium spinel down to 118 cm. A highly-deformed dunite domain cuts the harzburgite from 63-67 cm. Medium-grained granular gabbronorite veins 4-8mm wide crosscut the host harzburgite domain at 104cm and 116cm. One highly altered gabbroic vein (primary features obscured) is at 87cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic veinlet. The latter is made of secondary plagioclase, clinopyroxene, amphibole, prehnite, and chlorite. Bastite is green to grey, and black. Pink and white bastite could have formed after clinopyroxene. Spinel is fresh. "	"protogranular to porphyroclastic (20deg) serpentinized harzburgite with regular to strongly foliated mesh (10-20deg) with dunitic patches (shallow dips). Steep to moderately dipping magmatic veins, sub-horizontal picrolite veins cutting the magmatic veins, with shallow to moderately dipping white and magnetite veins (picrolite cuts magnetite veins)."	
"399"	"U1601"	"C"	"101"	"R"	"5"	""	"399-U1601C-101R-5"	"0.0"	"81.0"	"507.480"	"507.885"	"508.290"	"507.236"	"507.618"	"508"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 1% orthopyroxene, trace clinopyroxene and trace chromium spinel. Crosscut by medium-grained granular gabbronorite vein around 4mm wide at 2cm and 8cm."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veinlets. The latter is composed of secondary plagioclase, clinopyroxene, amphibole, prehnite, and chlorite. Bastite is green. The greenish patchy mesh contains white mesh centers whereas the dark mesh contains brown mesh centers."	"Protogranular to porphyroclastic (15deg) serpentinized harzburgite with regular mesh cut by moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"102"	"R"	"1"	""	"399-U1601C-102R-1"	"0.0"	"94.0"	"508.000"	"508.470"	"508.940"	"508"	"508.452"	"508.903"	""	"1, 2, 3, 4"	""	"Harzburgite with 17% orthopyroxene, trace clinopyroxene and trace chromium spinel down to 75 cm. Orthopyroxene has granular and interstitial textures. Pegmatitic gabbro with crystal size up to 6 cm is below a sharp but irregular contact with the harzburgite."	"Prehnite, talc, carbonate in coarse-grained gabbro. Prehnite is abundant at the contact with serpentinite."	"Protogranular serpentinized harzburgite with patchy regular mesh. isotropic gabbro interval with horizontal contact."	
"399"	"U1601"	"C"	"102"	"R"	"2"	""	"399-U1601C-102R-2"	"0.0"	"150.0"	"508.940"	"509.690"	"510.440"	"508.903"	"509.623"	"510.344"	""	"1, 2, 3, 4, 5"	""	"The top 9.5 cm is a continuation of the pegmatitic gabbro from the overlying section. The rest of the section is harzburgite with 17% orthopyroxene, trace chromium spinel and trace clinopyroxene."	"Highly serpentinized harzburgite cut by two hydrothermally altered magmatic veinlets. Gabbro is composed of Cpx, Plag, Amp, and secondary Plag, chlorite, and prehnite. The extent of alteration increases toward the serpentinite contact. The altered magmatic veins are composed of secondary plagioclase, clinopyroxene, amphibole, prehnite, and chlorite. Bastite is green to grey. Patchy alteration of the mesh."	"Protogranular serpentinized harzburgite with patchy regular mesh. isotropic, pegmatitic gabbro interval with sub-horizontal contact."	
"399"	"U1601"	"C"	"102"	"R"	"3"	""	"399-U1601C-102R-3"	"0.0"	"140.0"	"510.440"	"511.140"	"511.840"	"510.344"	"511.017"	"511.689"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Much of this section is harzburgite with both granular and interstitial orthopyroxene. Orthopyroxene proportions and grain sizes generally increase down section. The interval between 5 and 74.5 cm is pegmatitic gabbro. A 3 mm-wide gabbronorite vein centered at 114 cm cuts the harzburgite centered at 114 cm."	"Highly serpentinized harzburgite intruded by magmatic vein and altered gabbro. The latter is composed of plagioclase, secondary plagioclase, clinopyroxene, amphibole, prehnite, and chlorite. Bastite is green, grey. Spinel is unaltered."	"Protogranular serpentinized harzburgite with regular mesh. coarse grained isotropic gabbro interval with microfaults"	
"399"	"U1601"	"C"	"102"	"R"	"4"	""	"399-U1601C-102R-4"	"0.0"	"126.0"	"511.840"	"512.470"	"513.100"	"511.689"	"512.294"	"512.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Much of this section is harzburgite with both granular and interstitial orthopyroxene totaling about 18%. Trace chromium spinel is present.  The interval between 84 and 97 cm is pegmatitic gabbro. "	"Highly serpentinized harzburgite intruded by magmatic vein and altered gabbro. The latter is composed of plagioclase, secondary plagioclase, clinopyroxene, amphibole, prehnite, and chlorite. Bastite is green to grey."	"Protogranular serpentinized harzburgite with regular patchy mesh cut by pegmatitic isotropic gabbro, all cut by little white veins."	
"399"	"U1601"	"C"	"103"	"R"	"1"	""	"399-U1601C-103R-1"	"0.0"	"117.0"	"512.900"	"513.485"	"514.070"	"512.9"	"513.485"	"514.07"	""	"1"	""	"Much of this section is harzburgite with both granular and interstitial orthopyroxene totaling about 17%. Trace chromium spinel and clinopyroxene is present. The interval between 84 and 97 cm is pegmatitic gabbro."	"Highly serpentinized harzburgite with fresh spinel. Bastite is green to grey. Patch with greenish mesh."	"Protogranular serpentinized harzburgite with weakly foliated to regular patchy mesh cut by little white veins."	
"399"	"U1601"	"C"	"103"	"R"	"2"	""	"399-U1601C-103R-2"	"0.0"	"93.5"	"514.070"	"514.538"	"515.005"	"514.07"	"514.538"	"515.005"	""	"1, 2, 3"	""	"Harzburgite with 17% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel. Below 91 cm is coarse grained gabbro. This gabbro is likely the same generation as the pegmatitic gabbro in core 102, bit it is finer here because of its limited thickness."	"Highly serpentinized harzburgite cut by two hydrothermally overprinted magmatic veins composed of Cpx, plagioclase, secondary plagioclase, prehnite, and chlorite."	"Protogranular serpentinized harzburgite with regular patchy mesh cut by gabbro with moderate dip contact."	
"399"	"U1601"	"C"	"103"	"R"	"3"	""	"399-U1601C-103R-3"	"0.0"	"137.0"	"515.005"	"515.690"	"516.375"	"515.005"	"515.69"	"516.375"	""	"1"	""	"Harzburgite with 17% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel. The harzburgite is cut by an 8 mm wide gabbronorite vein at 115 cm."	"Highly serpentinized harzburgite cut by three hydrothermally overprinted magmatic veins composed of Cpx, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite."	"Protogranular serpentinized harzburgite with regular patchy mesh with modal, moderately dipping pyroxene contact in serpentinized harzburgite, cut by moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"103"	"R"	"4"	""	"399-U1601C-103R-4"	"0.0"	"124.0"	"516.375"	"516.995"	"517.615"	"516.375"	"516.995"	"517.615"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 18% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel.  The harzburgite is cut by an 8 mm wide gabbronorite vein at 4 cm."	"Highly serpentinized harzburgite cut by one hydrothermally overprinted magmatic vein composed of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is mostly green and in some instances grey. The serpentinized peridotite is cut by several types of veins including mesh, network of fibrous to massive chrysotile veins, and thick massive picrolite veins. The latter cut the magmatic vein."	"Protogranular to weakly porphyroclastic serpentinized harzburgite with regular patchy mesh to weakly foliated mesh moderate dipping magmatic vein and shallow little veins."	
"399"	"U1601"	"C"	"104"	"R"	"1"	""	"399-U1601C-104R-1"	"0.0"	"142.0"	"517.700"	"518.410"	"519.120"	"517.7"	"518.343"	"518.986"	""	"1, 2"	""	"Harzburgite with 17% orthopyroxene (granular and interstitial), 1% clinopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite. Bastite is mostly green and in some instances grey. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive picrolite veins."	"Protogranular serpentinized harzburgite with regular patchy mesh with little white veins dipping in opposite directions."	
"399"	"U1601"	"C"	"104"	"R"	"2"	""	"399-U1601C-104R-2"	"0.0"	"150.0"	"519.120"	"519.870"	"520.620"	"518.986"	"519.665"	"520.345"	""	"1, 2, 3, 4"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), 1% clinopyroxene and trace chromium spinel.  The harzburgite is cut by a gabbroic vein between 85 and 87 cm that is altered to the point that the original mineralogy and texture was not preserved. A dunite interval crosscuts the harzburgite from 129 to 134 cm."	"Highly serpentinized harzburgite cut by one hydrothermally overprinted magmatic vein composed of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is mostly green and in some instances grey. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by by serpentine-magnetite veins, fibrous to massive chrysotile veins, chrysotile-magnetite composite veins, and thick massive picrolite veins."	"Protogranular serpentinized harzburgite with regular patchy mesh, dunite layer with magnetite veins, moderate contact cut by moderately dipping magmatic vein."	
"399"	"U1601"	"C"	"104"	"R"	"3"	""	"399-U1601C-104R-3"	"0.0"	"139.0"	"520.620"	"521.315"	"522.010"	"520.345"	"520.975"	"521.604"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel. A dunite interval crosscuts the harzburgite from 44 to 48 cm."	"Highly serpentinized harzburgite and dunite. Bastite is mostly green and in some instances grey. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by by serpentine-magnetite veins, fibrous to massive chrysotile veins, and thick massive picrolite veins."	"Protogranular to poprphyroclastic serpentinized harzburgite with regular patchy mesh, dunite layer (shallow contact) with magnetite veins."	
"399"	"U1601"	"C"	"104"	"R"	"4"	""	"399-U1601C-104R-4"	"0.0"	"108.0"	"522.020"	"522.560"	"523.100"	"521.613"	"522.102"	"522.591"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with 17% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite. Bastite is mostly green and in some instances grey. In some areas, the mesh appears greenish. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, one thick chrysotile vein, and thick massive picrolite veins."	"Protogranular serpentinized harzburgite with regular patchy mesh cut by a horizontal white vein."	
"399"	"U1601"	"C"	"105"	"R"	"1"	""	"399-U1601C-105R-1"	"0.0"	"143.0"	"522.600"	"523.315"	"524.030"	"522.6"	"523.315"	"524.03"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace clinopyroxene and trace chromium spinel. The clinopyroxene increase towards 1% in the lower several cm, whereas the proportion orthopyroxene decreases. The harzburgite is cut by pegmatitic olivine-bearing gabbro between 20 and 139 cm. The contact is anastomosing contact and both igneous and reactionary. Olivine within the gabbro is derived from the harzburgite. Some areas have secondary minerals filling former porosity."	"Highly altered gabbro and highly serpentinized harzburgite cut by hydrothermally overprinted magmatic vein. The latter is made of amphibole, secondary plagioclase, prehnite, and chlorite. The gabbro is made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. Cut by chlorite, amphibole, zeolite, carbonate, and prehnite veins. Large grains of amphibole (primary?). Bastite is mostly green and in some instances grey. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with weak horizontal patchy mesh to no mesh, with multiple gabbro intervals, 65-70deg contacts, isotropic very altered."	
"399"	"U1601"	"C"	"105"	"R"	"2"	""	"399-U1601C-105R-2"	"0.0"	"150.0"	"524.040"	"524.790"	"525.540"	"524.04"	"524.79"	"525.54"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Harzburgite with 17% orthopyroxene (granular and interstitial), 1% clinopyroxene and trace chromium spinel. The harzburgite is black in the lower 16 cm. A medium-grained granular gabbro cuts the harzburgite from 109 to 134 cm."	"Highly serpentinized harzburgite and altered gabbro. The gabbro is made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. Gabbro is cut by chlorite, prehnite, and carbonate veins. Bastite is mostly green and becomes black towards the gabbro. The abundance of orthopyroxene decreases towards the gabbro. In some areas, the mesh appears greenish. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh, gabbro intervals with internal grain size contact with moderate dip."	
"399"	"U1601"	"C"	"105"	"R"	"3"	""	"399-U1601C-105R-3"	"0.0"	"142.0"	"525.550"	"526.260"	"526.970"	"525.55"	"526.26"	"526.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with 17% orthopyroxene and trace chromium spinel. Black between 63 and 82 cm. The basal 33 cm has coarse-grained granular gabbro."	"Highly serpentinized harzburgite and altered and bleached gabbro. The gabbro is made of amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Amphibole could be igneous. Gabbro is cut by prehnite, chlorite, and carbonate veins. Bastite is mostly green and becomes black towards the gabbro. The abundance of orthopyroxene decreases towards the gabbro. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular to weakly foliated (10-30deg) mesh, isotropic gabbro interval."	
"399"	"U1601"	"C"	"106"	"R"	"1"	""	"399-U1601C-106R-1"	"0.0"	"99.0"	"527.400"	"527.895"	"528.390"	"527.4"	"527.895"	"528.39"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. The top 12 cm has a course-grained gabbro domain, which is a continuation from the overlying section."	"Highly serpentinized harzburgite and altered and bleached gabbro. The gabbro is made of amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Amphibole could be igneous. Gabbro is cut by chlorite, prehnite, and carbonate veins. Bastite is mostly green to grey. The abundance of orthopyroxene decreases towards the gabbro. In some areas, the mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by several types of veins including mesh and a network of fibrous to massive chrysotile veins."	"Isotropic gabbro and protogranular serpentinized harzburgite with a regular mesh cut by little white veins (10deg) and a green vein (65deg)."	
"399"	"U1601"	"C"	"106"	"R"	"2"	""	"399-U1601C-106R-2"	"0.0"	"115.0"	"528.390"	"528.965"	"529.540"	"528.39"	"528.965"	"529.54"	""	"1, 2, 3"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. "	"Highly serpentinized harzburgite. Bastite is mostly green to grey. In some areas, mesh appears greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with regular mesh cut by little white veins (horizontal)."	
"399"	"U1601"	"C"	"106"	"R"	"3"	""	"399-U1601C-106R-3"	"0.0"	"144.0"	"529.540"	"530.260"	"530.980"	"529.54"	"530.26"	"530.98"	""	"1, 2, 3, 4"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. "	"Highly serpentinized harzburgite. Bastite is mostly green to grey. In some areas, the mesh appears greenish. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular to porphyroclastic (25-40deg) serpentinized harzburgite with regular to moderately foliated (30deg) mesh, cut by little white veins."	
"399"	"U1601"	"C"	"106"	"R"	"4"	""	"399-U1601C-106R-4"	"0.0"	"127.0"	"530.980"	"531.615"	"532.250"	"530.98"	"531.615"	"532.25"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene makes up the intervals from 0 to 30 and 76 to 127 cm. Dunite with 1% chromium spinel fills the central interval. Gabbronorite veins from 0.5 to 5 mm wide cut the core centered at 22, 27, 52, 61, and 73.5 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. It tends to be more greenish close to the dunite. The serpentinized peridotites are cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular to porphyroclastic (40deg) serpentinized harzburgite with regular to weakly foliated (40deg) mesh, dunite interval with 40deg contact, sub-parallel mesh, moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"107"	"R"	"1"	""	"399-U1601C-107R-1"	"0.0"	"150.0"	"532.300"	"533.050"	"533.800"	"532.3"	"533.05"	"533.8"	""	"1, 2, 3, 4"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. Two gabbronorite veins 1-4 mm wide cut the section centered at 5 and 46 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. It contains chlorite veins. Bastite is mostly green to grey. Mesh is locally greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Porphyroclastic (5deg) serpentinized harzburgite with regular mesh cut by moderately dipping magmatic veins and one green vein."	
"399"	"U1601"	"C"	"107"	"R"	"2"	""	"399-U1601C-107R-2"	"0.0"	"123.0"	"533.800"	"534.415"	"535.030"	"533.8"	"534.415"	"535.03"	""	"1"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. One gabbronorite veins about 7 mm wide cuts the section at 75 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. Mesh is locally greenish in patches. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"Protogranular to porphyroclastic (5deg) serpentinized harzburgite with regular to weakly foliated (25deg) mesh cut by little white veins."	
"399"	"U1601"	"C"	"107"	"R"	"3"	""	"399-U1601C-107R-3"	"0.0"	"137.0"	"535.040"	"535.725"	"536.410"	"535.04"	"535.725"	"536.41"	""	"1, 2"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. Mesh is locally greenish. The serpentinized peridotite is cut by serpentine-magnetite veins and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite with patchy regular to no mesh cut by shallowly dipping magmatic vein cut by slicked piece-end fault."	
"399"	"U1601"	"C"	"107"	"R"	"4"	""	"399-U1601C-107R-4"	"0.0"	"60.0"	"536.420"	"536.720"	"537.020"	"536.42"	"536.72"	"537.02"	""	"1, 2"	""	"Harzburgite with 20% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. A gabbronorite vein 3-4 mm thick crosscuts the core at a high angle between 14 and 43 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. Mesh is locally greenish. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"Protogranular serpentinized harzburgite with no mesh cut by steeply dipping magmatic vein."	
"399"	"U1601"	"C"	"108"	"R"	"1"	""	"399-U1601C-108R-1"	"0.0"	"150.0"	"537.100"	"537.850"	"538.600"	"537.1"	"537.798"	"538.495"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 18% orthopyroxene (granular and interstitial), trace chromium spinel, and trace clinopyroxene. A gabbronorite vein 2-3mm thick crosscuts the core at a high angle between 14 and 41 cm. Another  about 4 mm thick crosscuts the section centered at 114 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. Mesh is locally greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"Protogranular serpentinized harzburgite with patchy regular mesh cut by steeply dipping magmatic veins cut by gently dipping little white veins."	
"399"	"U1601"	"C"	"108"	"R"	"2"	""	"399-U1601C-108R-2"	"0.0"	"141.0"	"538.600"	"539.305"	"540.010"	"538.5"	"539.158"	"539.816"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 18% orthopyroxene, trace chromium spinel, and trace clinopyroxene. A gabbronorite vein 2-3mm thick crosscuts the core centered at 4 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The magmatic veins are made of clinopyroxene, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey. Mesh is locally greenish. Spinel is fresh. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"Protogranular serpentinized harzburgite with patchy regular mesh cut by moderately dipping magmatic vein cut by shallowly dipping little white veins."	
"399"	"U1601"	"C"	"108"	"R"	"3"	""	"399-U1601C-108R-3"	"0.0"	"121.0"	"540.010"	"540.615"	"541.220"	"539.816"	"540.38"	"540.945"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 18% orthopyroxene down to 105 cm. The interval between 21 and 28 cm as an orthopyroxene rich patch. The interval from 105-121 is coarse-grained granular gabbro with a dunitic upper contact with the harzburgite."	"Highly serpentinized harzburgite cut by hydrothermally altered gabbro. The latter is cut by prehnite, chlorite, and carbonate veins. The magmatic veins are made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green to grey with no talc. Spinel is partially altered to chlorite. The serpentinized peridotite is cut by serpentine-magnetite veins, fibrous to massive chrysotile veins, and massive picrolite veins."	"Protogranular serpentinized harzburgite with patchy regular mesh with gabbro and a contact with moderate dip cut by white-green veins."	
"399"	"U1601"	"C"	"108"	"R"	"4"	""	"399-U1601C-108R-4"	"0.0"	"113.0"	"541.220"	"541.785"	"542.350"	"540.945"	"541.472"	"542"	""	"1, 2, 3, 4, 5"	""	"The interval between 0 and 107 cm is coarse-grained granular gabbro with variable grain size. Below 107 cm is a small harzburgite domain. The boundary between the gabbro and harzburgite is troctolitic."	"Highly serpentinized dunite.  Variably altered gabbro with clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. The interval is cut by prehnite, chlorite, talc, and zeolite veins. "	"Isotropic gabbro, altered, with talc vein faults with a steep contact with serpentinized harzburgite."	
"399"	"U1601"	"C"	"109"	"R"	"1"	""	"399-U1601C-109R-1"	"0.0"	"127.0"	"542.000"	"542.635"	"543.270"	"542"	"542.626"	"543.252"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 15% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite. Bastite color varies from grey to green. Mesh is locally greenish. The very top piece is a highly altered gabbro, mostly altered plagioclase with a small amount of amphibole. Veins include serpentine-magnetite and chrysotile."	"Protogranular serpentinized harzburgite with patchy regular to weakly foliated (15deg) mesh."	
"399"	"U1601"	"C"	"109"	"R"	"2"	""	"399-U1601C-109R-2"	"0.0"	"141.0"	"543.270"	"543.975"	"544.680"	"543.252"	"543.947"	"544.641"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 17% orthopyroxene and trace chromium spinel."	"Highly serpentinzed harzburgite cut by a magmatic hydrothermal vein. The magmatic vein is comprised of Cpx, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Bastite color varies from greenish to grayish. The interval is cut by mesh, picrolite, and chrysotile veins."	"Protogranular serpentinized harzburgite with weakly foliated (15deg) to no mesh cut by shallowly dipping magmatic vein."	
"399"	"U1601"	"C"	"109"	"R"	"3"	""	"399-U1601C-109R-3"	"0.0"	"117.0"	"544.680"	"545.265"	"545.850"	"544.641"	"545.218"	"545.795"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 17% orthopyroxene and trace chromium spinel. Contains a gabbroic vein centered at 44 cm whose original mineral abundances and textures are obscured by alteration"	"Highly serpentinized harzburgite with hydrothermally altered gabbroic veins with Cpx, plagioclase, secondary plagioclase, prehnite, chlorite, and amphibole. Bastite is green to gray. Mesh is locally greenish. The interval is cut by serpentine-magnetite, chrysotile, and picrolite veins."	"Protogranular serpentinized harzburgite with no mesh to weakly foliated (15-20deg) mesh cut by sub-vertical magmatic vein."	
"399"	"U1601"	"C"	"109"	"R"	"4"	""	"399-U1601C-109R-4"	"0.0"	"102.0"	"545.850"	"546.360"	"546.870"	"545.795"	"546.298"	"546.8"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with c. 12 % orthopyroxene and trace spinel cut by several gabbroic veins. The largest vein is coarse-grained granular gabbro between 10 and 31 cm. Between 86 and 88 cm and the bottommost piece are highly altered gabbros whose primary features are obscured by alteration. A c. 4 mm thick medium-grained gabbronorite vein cuts the harzburgite centered at 38 cm"	"Highly serpentinized harzburgite, highly altered gabbro and gabbroic veins. Gabbro has Cpx, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Gabbro vein has Cpx, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Prehnite in gabbro is abundant at the contact with serpentinized harzburgite. Gabbro is crosscut by picrolite, prehnite, chlorite, and zeolite veins. Bastite is gray to black and locally green. The serpentinized harzburgite is cut by gabbro, serpentine-magnetite, and chrysotile veins."	"Protogranular serpentinized harzburgite no mesh. Gabbro interval, moderately dipping, with 2cm foliated zone and talc schist interval. Cut by moderately to steeply dipping magmatic veins cut by sub-normal green veins."	
"399"	"U1601"	"C"	"110"	"R"	"1"	""	"399-U1601C-110R-1"	"0.0"	"97.0"	"546.800"	"547.285"	"547.770"	"546.8"	"547.241"	"547.683"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is highly altered harzburgite with approzimatey 15 % orthopyroxene. A highly altered gabbro vein cuts the section at 36-37 cm."	"Highly serpentinized harzburgite with magmatic veins. The magmatic vein is gabbroic and has Cpx, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Green mesh could contain clay minerals. Bastite color varies from gray to green. The interval is cut by magmatic veins (gabbro), serpentine-magnetite, chrysotile, and picrolite veins."	"Protogranular serpentinized harzburgite, weakly foliated to no mesh cut by moderately dipping magmatic vein."	
"399"	"U1601"	"C"	"110"	"R"	"2"	""	"399-U1601C-110R-2"	"0.0"	"122.0"	"547.770"	"548.380"	"548.990"	"547.683"	"548.239"	"548.795"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with c. 15 % orthopyroxene. Has a diffuse veins centered at 116 cm which may represent impregnation of the harzburgite with gabbroic melts Also discrete altered gabbroic veins centered at 45 cm and 79 cm."	"Highly serpentinized harzburgite with magmatic veins. The magmatic vein is gabbro and has Cpx, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Mesh is locally greenish. Bastite color varies from gray to green and black. The interval is cut by serpentine-magnetite, chrysotile, picrolite, and magmatic (gabbro) veins."	"Protogranular to strongly porphyroclastic (20deg) serpentinized harzburgite, regular mesh to no mesh cut by several moderately dipping magmatic veins that are cut by perpendicular green veins."	
"399"	"U1601"	"C"	"110"	"R"	"3"	""	"399-U1601C-110R-3"	"0.0"	"146.0"	"548.990"	"549.720"	"550.450"	"548.795"	"549.46"	"550.124"	""	"1, 2, 3"	""	"Harzburgite with c. 15 % orthopyroxene. Has several diffuse veins, which may represent impregnation of the harzburgite with gabbroic melts (e.g., at 5 cm and 40 cm). Also discrete altered gabbroic veins at 71.5 cm and 103 cm."	"Highly serpentinized harzburgite cut by altered gabbroic veins. Highly altered bleached gabbro includes plagioclase, chlorite, zoisite, and epidote. The other gabbro veins include prehnite, chlorite, amphibole, plagioclase, secondary plagioclase, and Cpx. Mesh is locally greenish. Opx is relatively fresh. Hydrothermally altered magmatic veins are crosscut by picrolite veins in sets. The interval is also cut by serpentine-magnetite and chrysotile veins."	"Weakly porphyroclastic (0-15deg) serpentinized harzburgite, incipient mesh cut by moderately dipping magmatic veins."	
"399"	"U1601"	"C"	"110"	"R"	"4"	""	"399-U1601C-110R-4"	"0.0"	"124.0"	"550.450"	"551.070"	"551.690"	"550.124"	"550.689"	"551.254"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with c. 15 % orthopyroxene. Has a network of highly altered, diffuse gabbroic veins between 48 and 68 cm."	"Highly serpentinized harzburgite cut by altered gabbroic veins. The gabbro veins include prehnite, chlorite, amphibole, plagioclase, secondary plagioclase, and Cpx. Mesh is locally greenish. Hydrothermally altered magmatic veins are crosscut by picrolite-chrysotile composite veins. Bastite is gray, locally black. Opx is relatively fresh. The interval is also cut by serpentine-magnetite and chrysotile veins."	"Strongly porphyroclastic (20deg) serpentinized harzburgite, regular mesh cut by moderately dipping magmatic veins cut by normal green veins."	
"399"	"U1601"	"C"	"110"	"R"	"5"	""	"399-U1601C-110R-5"	"0.0"	"49.0"	"551.690"	"551.935"	"552.180"	"551.254"	"551.477"	"551.7"	""	"1"	""	"Harzburgite with c. 15 % orthopyroxene. Has a highly altered gabbro vein between centered at 26.5 cm. "	"Highly serpentinized harzburgite with gabbroic vein. The gabbroic vein has Cpx, plagioclase, secondary plagioclase, prehnite, and chlorite. Bastite is gray to black. The magmatic vein is cut by picrolite veins. The interval is also cut by serpentinite-magnetite and chrysotile veins."	"Weakly porphyroclastic (15deg) serpentinized harzburgite, regular mesh cut by a moderately dipping magmatic vein cut by normal green veins."	
"399"	"U1601"	"C"	"111"	"R"	"1"	""	"399-U1601C-111R-1"	"0.0"	"150.0"	"551.700"	"552.450"	"553.200"	"551.7"	"552.425"	"553.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Harzburgite with dunite intervals at 83-115 and 124-150 cm. The Harzburgite has less orthopyroxene towards the base, and chromium spinel throughout. The dunite intervals have 1-2% chromium spinel with relatively large grain sizes. A wherlite patch is present centered at c. 19 cm."	"Highly serpentinized harzburgite and dunite with a gabbroic vein in the serpentinized harzburgite. The gabbroic vein has Cpx, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. The magmatic vein is cut by picrolite veins. Spinel is relatively fresh. The section consists of serpentinized harzburgite between 9 and 82 cm. The serpentinized dunite from 82-150 lacks picrolite veins. The alteration style is similar for the serpentinized dunite and harzburgite. Bastite varies in color from gray to green. Mesh is locally greenish. The interval is also cut by chrysotile veins."	"Protogranular serpentinized harzburgite, dunite intervals, pyroxenite interval, regular mesh with shallow to moderate contact dips cut by moderate to steeply dipping magmatic veins cut by normal green veins."	
"399"	"U1601"	"C"	"111"	"R"	"2"	""	"399-U1601C-111R-2"	"0.0"	"150.0"	"553.200"	"553.950"	"554.700"	"553.15"	"553.875"	"554.601"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The upper 86.5 cm consists of medium grained olivine gabbro with about 5% patches of troctolite. Harzburgite with about 12 % orthopyroxene and trace spinel makes up most of the rest of the section. This harzburgite is cut by a medium grained olivine gabbro between 119 and 139.5 cm. This gabbro has a troctolitic reaction boundary at the lower contact."	"Highly serpentinized Opx-bearing dunite with highly altered gabbro. The gabbro vein has Cpx, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. The altered gabbro is at the top and bottom of the section with the serpentinized Opx-bearing dunite in between. Alteration of the gabbro is variable. Bastite is gray to black."	"Intervals of gabbro within protogranular serpentinized harzburgite no mesh with moderate contact dips cut by green-talc veins and one faulted vein."	
"399"	"U1601"	"C"	"111"	"R"	"3"	""	"399-U1601C-111R-3"	"0.0"	"142.0"	"554.700"	"555.410"	"556.120"	"554.6"	"555.287"	"555.973"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Orthopyroxene-poor harzburgite and orthopyroxene-bearing dunite with trace chromium spinel down to 23.5 cm. The rest of the section is harzburgite with c. 20 % orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite and Opx-bearing dunite (upper part of the section). Bastite is grey to green. Greenish mesh in dunite and locally in harzburgite. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"Protogranular to porphyroclastic (0deg) serpentinized harzburgite, with dunite, regular mesh cut by little white veins."	
"399"	"U1601"	"C"	"111"	"R"	"4"	""	"399-U1601C-111R-4"	"0.0"	"54.5"	"556.120"	"556.393"	"556.665"	"555.973"	"556.237"	"556.502"	""	"1, 2, 3, 4"	""	"Most of the section is harzburgite with c. 20 % orthopyroxene and trace chromium spinel. A heavily altered gabbro vein cuts the section at c. 39 cm. Pebbles of this gabbro are found at the base of the section."	"Highly serpentinized harzburgite cut by one hydrothermally overprinted magmatic vein made of secondary plagioclase, amphibole, prehnite, chlorite, and possibly epidote. Bastite is black to green. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and a set of massive white serpentine veins."	"Protogranular serpentinized harzburgite, regular mesh cut by magnetite veins cut by white veins"	
"399"	"U1601"	"C"	"112"	"R"	"1"	""	"399-U1601C-112R-1"	"0.0"	"150.0"	"556.500"	"557.250"	"558.000"	"556.5"	"557.223"	"557.947"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with minimal orthopyroxene grading downward to dunite. Trace chromium spinel is found throughout. The lowermost 10 cm is a pervasively altered gabbro. A vein of this same material is centered at 118.5 cm."	"Highly serpentinized harzburgite and dunite are cut by two hydrothermally overprinted magmatic veins made of plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Altered gabbro is composed of clinopyroxene, plagioclase, secondary plagioclase, prehnite, and chlorite. Clinopyroxene is replaced by clays (? reddish brown material). Gabbro is cut by chlorite and prehnite-carbonate veins. Bastite is grey to green, minor black. In dunite, bastite tends to be black. Mesh is locally green in harzburgite. Spinel is fresh. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and a set of massive picrolite serpentine veins."	"Protogranular to porphyroclastic (0deg) serpentinized harzburgite, with dunite and gabbro, regular mesh. Gabbro dunite contact is faulted and steep on one side and steeply dipping on the other side."	
"399"	"U1601"	"C"	"112"	"R"	"2"	""	"399-U1601C-112R-2"	"0.0"	"150.0"	"558.000"	"558.750"	"559.500"	"557.947"	"558.67"	"559.394"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Harzburgite with 12% orthopyroxene, and trace clinopyroxene and chromium spinel. An altered gabbro vein steeply cuts the top of the section."	"Highly serpentinized Opx-bearing dunite to harzburgite. The latter is cut by two hydrothermally overprinted magmatic veins made of plagioclase, clinopyroxene, secondary plagioclase, amphibole, prehnite, and chlorite. Sulfide-oxyhydroxide veins form a network in the dunite. Bastite is black and rimmed by bronze to green corona. Mesh is brown and black. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, a set of serpentine-carbonate serpentine veins, sulfide-carbonates veins, and sulfides-oxyhydroxide veins."	"Protogranular serpentinized harzburgite, no mesh to weakly foliated (0deg) mesh cut by steeply dipping magmatic veins."	
"399"	"U1601"	"C"	"112"	"R"	"3"	""	"399-U1601C-112R-3"	"0.0"	"150.0"	"559.500"	"560.250"	"561.000"	"559.394"	"560.117"	"560.841"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Harzburgite with 10% orthopyroxene, and trace clinopyroxene and chromium spinel to 93.5 cm. A course-grained seriate gabbro makes up the rest of the section. The gabbro has a olivine-bearing reaction boundary against peridotite, which is orthopyroxene-poor near this boundary."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally overprinted magmatic vein made of plagioclase, clinopyroxene, secondary plagioclase, amphibole, prehnite, and chlorite. Highly altered gabbro made of plagioclase, clinopyroxene, secondary plagioclase, amphibole, prehnite, and chlorite. Cut by chlorite-prehnite and talc-carbonate veins. Bastite is black to grey. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, a set of massive picrolite veins, and sulfide-carbonates veins."	"Protogranular serpentinized harzburgite, reg mesh, isotropic gabbro with steep contact."	
"399"	"U1601"	"C"	"112"	"R"	"4"	""	"399-U1601C-112R-4"	"0.0"	"58.0"	"561.000"	"561.290"	"561.580"	"560.841"	"561.12"	"561.4"	""	"1, 2, 3, 4, 5"	""	"The  gabbro in the base of the overlying section continues through 20 cm, where it has a reaction boundary with the underlying harzburgite similar to that of the overlying section."	"Highly serpentinized harzburgite with a variable abundance of orthopyroxene. Highly altered gabbro made of plagioclase, clinopyroxene, secondary plagioclase, amphibole, prehnite, and chlorite. It is cut by talc-carbonate, chlorite, and zeolite veins. Bastite is green. Spinel is fresh. The serpentinites are crosscut by several types of veins including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and a set of massive white to green serpentine veins."	"Protogranular serpentinized harzburgite, reg mesh, isotropic gabbro intruded by moderately dipping leuco-magmatic vein with sheared dark green veins. All cut by white-green veins."	
"399"	"U1601"	"C"	"113"	"R"	"1"	""	"399-U1601C-113R-1"	"0.0"	"118.0"	"561.400"	"561.990"	"562.580"	"561.4"	"561.962"	"562.524"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with both granular and interstitial orthopyroxene totaling 20%; also contains trace clinopyroxene and spinel."	"Highly serpentinized harzburgite. Bastite is green to grey. The mesh is green. Spinel is fresh. Piece 6 contains picrolite slickenside. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Protogranular serpentinized harzburgite, patchy reg mesh cut by little white veins with steepening dip."	
"399"	"U1601"	"C"	"113"	"R"	"2"	""	"399-U1601C-113R-2"	"0.0"	"136.0"	"562.580"	"563.260"	"563.940"	"562.524"	"563.172"	"563.819"	""	""	""	"Harzburgite with both granular and interstitial orthopyroxene totaling 20%; also contains trace clinopyroxene and spinel."	"Highly serpentinized harzburgite. Bastite is green to grey. The mesh is green. Spinel is fresh. Piece 6 contains picrolite slickenside. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Weakly foliated, regular mesh serpentinized harzburgite cut by steep magnetite vein."	
"399"	"U1601"	"C"	"113"	"R"	"3"	""	"399-U1601C-113R-3"	"0.0"	"131.0"	"563.940"	"564.595"	"565.250"	"563.819"	"564.443"	"565.067"	""	"1, 2, 3, 4"	""	"Harzburgite with both granular and interstitial orthopyroxene totaling 20%; also contains trace clinopyroxene and spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of plagioclase, secondary plagioclase, prehnite, chlorite, and amphibole. Bastite is green-grey, becoming black downsection. The serpentinite contains distinct vein types, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins."	"Porphyroclastic to protogranular (10deg) serpentinized harzburgite, regular mesh. Several carbonate veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"113"	"R"	"4"	""	"399-U1601C-113R-4"	"0.0"	"119.0"	"565.250"	"565.845"	"566.440"	"565.067"	"565.634"	"566.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with both granular and interstitial orthopyroxene totaling 20%; also contains trace clinopyroxene and spinel. This section is cut by a coarse-grained gabbro domain between 13 and 56 cm. The gabbro has a troctolitic reaction boundary with the harzburgite."	"Highly serpentinized harzburgite and altered gabbro (7-60cm). Bastite is grey to green. The mesh is black. No spinel is visible. Partiall serpentinized olivine xenocrysts in gabbro near harzburgite contact. The serpentinite contains distinct vein types, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins. Gabbro contains chlorite-carbonate veins."	"Protogranular serpentinized harzburgite, patchy regular mesh, gabbro interval, undeformed, isotropic"	
"399"	"U1601"	"C"	"114"	"R"	"1"	""	"399-U1601C-114R-1"	"0.0"	"133.0"	"566.200"	"566.865"	"567.530"	"566.2"	"566.798"	"567.396"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with c. 17 % orthopyroxene with both granular and interstitial textures; trace clinopyroxene and chromium spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of plagioclase, prehnite, chlorite, and amphibole. Bastite green-grey. Spinel is unaltered. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Protogranular serpentinized harzburgite, patchy regular mesh."	
"399"	"U1601"	"C"	"114"	"R"	"2"	""	"399-U1601C-114R-2"	"0.0"	"122.0"	"567.530"	"568.140"	"568.750"	"567.396"	"567.944"	"568.493"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with c. 17 % orthopyroxene with both granular and interstitial textures; trace clinopyroxene and chromium spinel."	"Highly serpentinized Hz. Bastite is green to grey. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Protogranular serpentinized harzburgite, regular to weakly foliated very patchy mexh"	
"399"	"U1601"	"C"	"114"	"R"	"3"	""	"399-U1601C-114R-3"	"0.0"	"142.0"	"568.750"	"569.460"	"570.170"	"568.493"	"569.131"	"569.769"	""	"1"	""	"Harzburgite with c. 17 % orthopyroxene with both granular and interstitial textures; trace clinopyroxene and chromium spinel."	"Highly serpentinized harzburgite with green-grey bastite and green-black mesh. Spinel is fresh. Greenish mesh is present in patches. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite, regular to weakly foliated mesh 50(deg)"	
"399"	"U1601"	"C"	"114"	"R"	"4"	""	"399-U1601C-114R-4"	"0.0"	"146.0"	"570.190"	"570.920"	"571.650"	"569.787"	"570.443"	"571.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with c. 17 % orthopyroxene with both granular and interstitial textures; trace clinopyroxene and chromium spinel."	"Highly serpentinized harzburgite with green-grey bastite and green-black mesh. Spinel is fresh. Patchy alteration cause greenish mesh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins. (same as 114R-3)"	"Protogranular serpentinized harzburgite, regular to no mesh"	
"399"	"U1601"	"C"	"115"	"R"	"1"	""	"399-U1601C-115R-1"	"0.0"	"113.0"	"571.100"	"571.665"	"572.230"	"571.1"	"571.665"	"572.23"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 18% orthopyroxene and trace spinel down to 99.5 cm. Dunite with 1% rounded chromium spinel grains is beneath."	"Highly serpentinized harzburgite and minor dunite. Green-grey bastite and green-black mesh in harzburgite and green mesh in dunite. Spinel is fresh. Patchy alteration of greenish mesh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and white picrolite vein. One chlorite vein."	"Weakly porphyroclastic serpentinized harzburgite (0deg), dunite interval, regular mesh, poorly formed little white veins with crosscutting orientations (5-30deg)."	
"399"	"U1601"	"C"	"115"	"R"	"2"	""	"399-U1601C-115R-2"	"0.0"	"130.0"	"572.230"	"572.880"	"573.530"	"572.23"	"572.88"	"573.53"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Dunite with 1% rounded chromium spinel grains continued from the overlying section overlies harzburgite with c. 18% orthopyroxene and trace spinel. The lowermost 24 cm is coarse-grained and granular gabbro."	"Highly serpentinized harzburgite and dunite, and altered gabbro. Gabbro contains amphibole after Cpx, plagioclase altered to chlorite, and secondary plagioclase. The extent of alteration in gabbro increases at the contact with serpentinite. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and white massive serpentine veins. Gabbro contains prehnite-chlorite-carbonate veins."	"Protogranular serpentinized harzburgite, dunite interval, reg mesh, gabbro, isotropic, fractured."	
"399"	"U1601"	"C"	"115"	"R"	"3"	""	"399-U1601C-115R-3"	"0.0"	"90.0"	"573.530"	"573.980"	"574.430"	"573.53"	"573.98"	"574.43"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"The uppermost 51cm is coarse-grained and granular gabbro. It is underlain by overlies dark, heavily altered harzburgite with c. 15% orthopyroxene, trace spinel, and trace clinopyroxene. "	"Altered gabbro and highly serpentinized harzburgite. Mesh is black. Bastite is white to grey to black. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. One massive serpentine vein turns into a composite serpentine-carbonate sulfide vein."	"Gabbro above serpentinized harzburgite with no mesh. Green curvey vein modifies local mesh."	
"399"	"U1601"	"C"	"116"	"R"	"1"	""	"399-U1601C-116R-1"	"0.0"	"140.0"	"575.900"	"576.600"	"577.300"	"575.9"	"576.561"	"577.222"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Dunite with a few % orthopyroxene and trace clinopyroxene near the top. Trace chromium spinel is present throughout the ultramafic portion of this section. The interval from 10.5 to 136 cm is coarse-grained gabbro with highly varied grain size (2-34 mm) and trace sulfides. "	"Moderately altered gabbro and highly serpentinized Opx-bearing dunite. Olivine in melt-impregnated dunite is partially serpentinized (117-127 cm). Mesh is black. Bastite is black and grey. Gabbro contains (mm-sized) disseminated sulfide. Gabbro is more altered close to the serpentinite. Mesh texture in serpentinized dunite is black-brown and cut by sulfide veins."	"Serpentinized harzburgite/serpentinite and isotropic gabbro, some microfaulting in gabbro."	
"399"	"U1601"	"C"	"116"	"R"	"2"	""	"399-U1601C-116R-2"	"0.0"	"150.0"	"577.300"	"578.050"	"578.800"	"577.222"	"577.93"	"578.638"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The dunite from the overlying section continues for the first 4.5 cm. It is underlain by harzburgite with orthopyroxene averaging  about 12% and trace clinopyroxene. The harzburgite is cut by a network of pervasively altered gabbro veins with primary properties obscured. "	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of chlorite, amphibole, prehnite, clinopyroxene, and primary and secondary plagioclase. Bastite is green to grey. Mesh is black. Spinel is fresh. Talc-tremolite-chlorite vein in serpentinite. "	"Protogranular serpentinized harzburgite, dunite, no mesh, lots of magmatic veins, maybe sheared."	
"399"	"U1601"	"C"	"116"	"R"	"3"	""	"399-U1601C-116R-3"	"0.0"	"138.0"	"578.800"	"579.490"	"580.180"	"578.638"	"579.289"	"579.941"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Most of this section is harzburgite averaging 15 % orthopyroxene and with trace clinopyroxene. Thin gabbro veins cut through the harzburgite centered at 38, 53, and 102.5 cm. The basal 22 cm is orthopyroxene-bearing dunite with trace spinel."	"Highly serpentinized Opx-bearing dunite and harzburgite. Bastite is grey to green. Mesh is greenish to black. Spinel is fresh. Dunite is cut by two hydrothermally altered magmatic veins composed of amphibole, primary and secondary plagioclase, chlorite, and prehnite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and massive white serpentine veins."	"Protogranular to weakly porphyroclastic serpentinized harzburgite (10deg) with no mesh to regular spotty green mesh. Steep little white veins."	
"399"	"U1601"	"C"	"116"	"R"	"4"	""	"399-U1601C-116R-4"	"0.0"	"91.0"	"580.180"	"580.635"	"581.090"	"579.941"	"580.37"	"580.8"	""	"1, 2, 3"	""	"Most of this section is harzburgite averaging 15 % orthopyroxene and with trace clinopyroxene. Highly altered cm-scale gabbro veins cut through the harzburgite centered at 42 and 67 cm. "	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein composed of Cpx, plagioclase, amphibole, chlorite, secondary plagioclase, and prehnite. Mesh is black and minor green. Bastite is green and grey. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Serpentinized harzburgite with magmatic veins, significant alteration, sheared talc tremolite (?) vein contacts."	
"399"	"U1601"	"C"	"117"	"R"	"1"	""	"399-U1601C-117R-1"	"0.0"	"139.0"	"580.800"	"581.495"	"582.190"	"580.8"	"581.495"	"582.19"	""	"1, 2, 3, 4"	""	"Harzburgite with patches that may contain fresh olivine. This interval has 18% orthopyroxene and trace clinopyroxene and spinel. A highly-altered gabbro domain cuts nearly vertically down the core from 0-67 cm. Another altered gabbro vein cuts the harzburgite centered at 131 cm."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of prehnite, chlorite amphibole, secondary plagioclase, epidote, and carbonate. Primary plagioclase and clinopyroxene (rodingite, 0-66 cm)."	"Protogranular serpentinized harzburgite with mesh to regular mesh. Schistose magmatic veins with strong foliated shear fabric and breccia."	
"399"	"U1601"	"C"	"117"	"R"	"2"	""	"399-U1601C-117R-2"	"0.0"	"150.0"	"582.190"	"582.940"	"583.690"	"582.19"	"582.94"	"583.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The uppermost 46 cm is harzburgite  with c. 12 % orthopyroxene cut by a highly altered gabbro vein centered at 25 cm. Between 47 and 51 cm is a medium-grained gabbro with interstitial clinopyroxene. The rest of the section is harzburgite with orthopyroxene averaging c. 17 % and trace chromium spinel. This part of the section is cut by altered gabbro veins centered at 68, 110, and 126 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of plagioclase, clinopyroxene, prehnite, chlorite, amphibole, and secondary plagioclase. Bastite is grey and locally green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Strongly foliated serpentinized harzburgite (15-30deg) with no mesh. Several of magmatic veins."	
"399"	"U1601"	"C"	"117"	"R"	"3"	""	"399-U1601C-117R-3"	"0.0"	"145.0"	"583.690"	"584.415"	"585.140"	"583.69"	"584.415"	"585.14"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The upper 103 cm is harzburgite with 15 % orthopyroxene and trace spinel. Dunite with trace spinel is below. Coarse-grained gabbros with troctolitic reaction borders, cut the section centered at 102 and from 116 onward. "	"Highly serpentinized harzburgite and dunite. Highly altered gabbro. The harzburgite is cut by a hydrothermally altered magmatic vein composed of plagioclase, clinopyroxene, prehnite, chlorite, amphibole, and secondary plagioclase. Same assemblage in the gabbro. It is rich in prehnite at the contact with the dunite. Gabbro is cut by chlorite veins. Bastite is green and grey and becomes black close to the dunite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins."	"Strongly foliated serpentinized harzburgite (20deg), no mesh, dunite, isotropic gabbro interval."	
"399"	"U1601"	"C"	"118"	"R"	"1"	""	"399-U1601C-118R-1"	"0.0"	"145.0"	"585.600"	"586.325"	"587.050"	"585.6"	"586.321"	"587.041"	""	"1, 2, 3, 4, 5, 6, 7"	""	"0-13 cm - Gabbro similar to that in the overlying section, with dunite beneath a contact. The dunite is mixed with an older, more altered generation of gabbro."	"Highly serpentinized harzburgite and altered gabbro (0-13 cm). The gabbro is made of plagioclase, clinopyroxene, prehnite, chlorite, amphibole, and secondary plagioclase. It is cut by chlorite-prehnite veins. The harzburgite is cut by a hydrothermally altered magmatic vein composed of plagioclase, prehnite, chlorite, amphibole, secondary plagioclase, and a brownish mineral (zoisite?). Bastite is green, grey, and black without tendency. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. The latter cut through the magmatic veins."	"Gabbro above stongly foliated serpentinized harzburgite with no mesh. Several of altered magmatic veins. Altered veins are cut by fresher gabbro."	
"399"	"U1601"	"C"	"118"	"R"	"2"	""	"399-U1601C-118R-2"	"0.0"	"150.0"	"587.050"	"587.800"	"588.550"	"587.041"	"587.787"	"588.532"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene. Several gabbro veins and areas cut the harzburgite, including within the uppermost 18 cm, ane between 108 cm and the base of the section. This gabbro is highly altered, but some of its original characteristics are preserved. Its granular texture is particularly well preserved at the base of the section."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase, prehnite, chlorite, amphibole, and secondary plagioclase. Bastite is grey to black. Some domains with fresh olivine (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins grading to carbonate when entering in the magmatic vein. Picrolite-carbonate, chlorite, and prehnite veins cut through the magmatic vein."	"Strongly foliated serpentinized harzburgite (20deg), no mesh, schistose vein with vertical dip-slip shear sense."	
"399"	"U1601"	"C"	"118"	"R"	"3"	""	"399-U1601C-118R-3"	"0.0"	"111.0"	"588.550"	"589.105"	"589.660"	"588.532"	"589.083"	"589.635"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene. A gabbro domain cuts the harzburgite through much of the first 63 cm. This gabbro is highly altered, but some of its original characteristics are preserved. It fines down section."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase, prehnite, chlorite, amphibole, and secondary plagioclase. Bastite is green and grey. Some domains with fresh olivine (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. Picrolite, chlorite, and carbonate veins cut through the magmatic vein."	"Foliated serpentinized harzburgite (20deg), no mesh, schistose sheared vein"	
"399"	"U1601"	"C"	"118"	"R"	"4"	""	"399-U1601C-118R-4"	"0.0"	"87.0"	"589.660"	"590.095"	"590.530"	"589.635"	"590.067"	"590.5"	""	"1, 2, 3, 4, 5, 6"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene and chromium spinel. A thin, highly-altered gabbro vein cuts the harzburgite from much of 16-60 cm.  "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase, prehnite, chlorite, and secondary plagioclase. Bastite is grey and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic vein."	"Strongly foliated serpentinized harzburgite (20deg), patchy regular mesh."	
"399"	"U1601"	"C"	"119"	"R"	"1"	""	"399-U1601C-119R-1"	"0.0"	"136.0"	"590.500"	"591.180"	"591.860"	"590.5"	"591.18"	"591.86"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene and chromium spinel. A thin, highly-altered gabbro vein cuts the harzburgite centered at 27, 70, and 128 cm."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, prehnite, chlorite, and secondary plagioclase. Bastite is grey and black. Locally greenish mesh domains. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic vein."	"Weakly foliated serpentinized harzburgite (0-25deg), patchy regular to weakly foliated mesh. Green vein faulted by sub-vertical normal fault 10cm offset. Fault and green vein is cross-cut by local little white veins."	
"399"	"U1601"	"C"	"119"	"R"	"2"	""	"399-U1601C-119R-2"	"0.0"	"118.0"	"591.860"	"592.450"	"593.040"	"591.86"	"592.45"	"593.04"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene and chromium spinel. A thin, highly-altered gabbro vein cuts the harzburgite centered at 25 cm. A medium-grained gabbro domain is present at the base of the section."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, prehnite, chlorite, and secondary plagioclase. Locally greenish mesh domains. Bastite is grey and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. Picrolite, chlorite, and zeolite veins cut through the magmatic vein."	"Weakly foliated serpentinized harzburgite (10deg), patchy regular mesh, magmatic veins."	
"399"	"U1601"	"C"	"119"	"R"	"3"	""	"399-U1601C-119R-3"	"0.0"	"130.0"	"593.040"	"593.690"	"594.340"	"593.04"	"593.69"	"594.34"	""	"1, 2, 3, 4, 5"	""	"Harzburgite, most of the orthopyroxene is granular; interstitial orthopyroxene is present This section has slightly more Cr-spinel than in sections 1-2. "	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of chlorite and a white mineral. Bastite is grey and green. Some domains with relicts of olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic vein."	"Weakly foliated serpentinized harzburgite (20deg), patchy regular mesh."	
"399"	"U1601"	"C"	"119"	"R"	"4"	""	"399-U1601C-119R-4"	"0.0"	"74.0"	"594.340"	"594.710"	"595.080"	"594.34"	"594.71"	"595.08"	""	"1, 2, 3"	""	"Harzburgite, most of the orthopyroxene is granular; interstitial orthopyroxene is present This section has slightly more Cr-spinel than in sections 1-2. "	"Moderately to highly serpentinized harzburgite. Bastite is mostly grey and locally green. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"Strongly foliated serpentinized harzburgite (20deg), regular mesh."	
"399"	"U1601"	"C"	"120"	"R"	"1"	""	"399-U1601C-120R-1"	"0.0"	"144.0"	"595.300"	"596.020"	"596.740"	"595.3"	"595.993"	"596.686"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with 15 % orthopyroxene and trace clinopyroxene and chromium spinel down to 117 cm. Medium-grained gabbro veins crosscutting the host harzburgite at 14cm and 80cm. The interval from 117-137 cm is a gabbro with a troctolitic lower boundary. The lowermost piece is a dunite with trace spinel"	"Moderately to highly serpentinized harzburgite and dunite. The harzburgite is cut by a hydrothermally altered magmatic vein composed of clinopyroxene, secondary plagioclase, prehnite, amphibole, and chlorite. Altered gabbro (116-137 cm) at the contact with serpentinized dunite. Gabbro is made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Mesh is locally greenish. Bastite is mostly grey and locally green. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic vein."	"Strongly foliated serpentinized harzburgite (20deg), patchy regular mesh, gabbro interval."	
"399"	"U1601"	"C"	"120"	"R"	"2"	""	"399-U1601C-120R-2"	"0.0"	"140.0"	"596.750"	"597.450"	"598.150"	"596.696"	"597.37"	"598.044"	""	"1, 2, 3, 4, 5"	""	"The dunite from the overlying section continues into the uppermost piece. The rest of the section is harzburgite"	"Moderately to highly serpentinized harzburgite and dunite. The harzburgite is cut by a hydrothermally altered magmatic vein composed of clinopyroxene, secondary plagioclase, prehnite, and chlorite. Mesh is locally greenish. Bastite is mostly grey and locally green. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"Protogranular to weakly foliated serpentinized harzburgite (0deg), dunite, patchy regular mesh."	
"399"	"U1601"	"C"	"120"	"R"	"3"	""	"399-U1601C-120R-3"	"0.0"	"128.0"	"598.150"	"598.790"	"599.430"	"598.044"	"598.66"	"599.276"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"A coarse gabbro is at the top of the section. Dunite underlies the gabbro down to 31 cm. The rest of the section is harzburgite with c. 15 % orthopyroxene and trace spinel."	"Moderately to completely serpentinized harzburgite and dunite. Altered gabbro (0-8 cm) at the contact with serpentinized dunite. The gabbro is made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. It contains partly serpentinized olivine xenocrysts close to the contact with the dunite. It is cut by chlorite veins that turn to serpentine when propagating in the serpentinized dunite. Mesh is brown-black and contains disseminated sulfides in places, while it is locally greenish. Bastite is mostly grey and locally green. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"Protogranular to weakly foliated serpentinized harzburgite (10deg), dunite, patchy regular mesh, weakly magmatically foliated gabbro interval"	
"399"	"U1601"	"C"	"120"	"R"	"4"	""	"399-U1601C-120R-4"	"0.0"	"96.0"	"599.430"	"599.910"	"600.390"	"599.276"	"599.738"	"600.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The section is dominantly harzburgite with minimal orthopyroxene. A gabbro metamorphosed to amphibolite crosscuts the section between 77 and 94 cm. "	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of secondary plagioclase, prehnite, and chlorite. The proportion of orthopyroxene decreases towards the gabbro. Altered gabbro (74-96 cm) is made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. It is cut by amphibole and prehnite-carbonate veins that transition to picrolite in dunite. The mesh is greenish. Bastite is mostly grey, green, and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic vein."	"Protogranular serpentinized harzburgite. Gabbro interval is mylonite shear zone opx have sheared wings."	
"399"	"U1601"	"C"	"121"	"R"	"1"	""	"399-U1601C-121R-1"	"0.0"	"139.0"	"600.200"	"600.895"	"601.590"	"600.2"	"600.882"	"601.564"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Harzburgite with c. 10% orthopyroxene and trace chromium spinel. There are pervasively altered thin veins of gabbro cutting the harzburgite in the upper 40 cm. A medium-grained gabbroic intrusion cuts the section from 40-50 cm."	"Highly to completely serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, amphibole, and chlorite. Bastite is mostly grey, green, and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Protogranular serpentinized harzburgite with patchy regular mesh."	
"399"	"U1601"	"C"	"121"	"R"	"2"	""	"399-U1601C-121R-2"	"0.0"	"144.0"	"601.590"	"602.310"	"603.030"	"601.564"	"602.271"	"602.978"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with c. 10% orthopyroxene and trace chromium spinel. Pervasively altered thin veins of gabbro up to 18 mm wide cut the harzburgite primarily centered at 99 and 128 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite. The former is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, amphibole, chlorite, and a brownish mineral. The mesh is black and locally greenish. Bastite is grey, green, and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Protogranular to porphyroclastic (10deg) serpentinized harzburgite, no mesh to regular mesh, red-green altered magmatic vein."	
"399"	"U1601"	"C"	"121"	"R"	"3"	""	"399-U1601C-121R-3"	"0.0"	"127.0"	"603.030"	"603.665"	"604.300"	"602.978"	"603.601"	"604.224"	""	"1, 2"	""	"Harzburgite with c. 11% orthopyroxene and trace chromium spinel. Proportions of orthopyroxene vary on a 10 cm scale."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein made of prehnite, amphibole, and chlorite. The mesh is black and locally greenish. Bastite is grey, green, and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Strongly porphyroclastic (0deg) serpentinized harzburgite, moderately foliated mesh (40-45deg)."	
"399"	"U1601"	"C"	"121"	"R"	"4"	""	"399-U1601C-121R-4"	"0.0"	"56.0"	"604.530"	"604.810"	"605.090"	"604.45"	"604.725"	"604.999"	""	"1, 2, 3"	""	"Harzburgite with c. 11% orthopyroxene and trace chromium spinel. Proportions of orthopyroxene vary on a 10 cm scale. A highly altered gabbro vein is present at the base of the section."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of plagioclase, secondary plagioclase, prehnite, amphibole, and chlorite. The mesh is black and locally greenish. Bastite is grey and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Strongly porphyroclastic (10deg) serpentinized harzburgite, moderately foliated mesh (30deg)."	
"399"	"U1601"	"C"	"122"	"R"	"1"	""	"399-U1601C-122R-1"	"0.0"	"141.0"	"605.000"	"605.705"	"606.410"	"605"	"605.644"	"606.287"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with c. 11% orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of prehnite, amphibole, and chlorite. Mesh turns from greenish-black to brownish-black down section. Bastite turns from dark green to dark green with a brown corona down section. Spinel displays a yellowish luster down section. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Strongly porphyroclastic (0deg) serpentinized harzburgite, weakly foliated mesh (0deg)"	
"399"	"U1601"	"C"	"122"	"R"	"2"	""	"399-U1601C-122R-2"	"0.0"	"115.0"	"606.410"	"606.985"	"607.560"	"606.287"	"606.812"	"607.336"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with c. 11% orthopyroxene and trace chromium spinel. A medium-grained granular gabbro cuts the harzburgite between 85 and 90 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, amphibole, and chlorite. Mesh is locally greenish. Bastite is grey, black, and green. Spinel is fresh. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Protogranular serpentinized harzburgite, regular mesh."	
"399"	"U1601"	"C"	"122"	"R"	"3"	""	"399-U1601C-122R-3"	"0.0"	"141.0"	"607.560"	"608.265"	"608.970"	"607.336"	"607.98"	"608.623"	""	"1, 2, 3, 4"	""	"Harzburgite with c. 12% orthopyroxene and trace chromium spinel. Beneath 127 cm is an olivine gabbro, where the olivine appears to have been derived from the peridotite."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, prehnite, amphibole, and chlorite. Altered gabbro (128-139 cm) containing possibly serpentinized olivine xenocrysts. The mesh is black and locally greenish. Bastite is grey and black. Spinel is fresh. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Weakly porphyroclastic (0deg) to protogranular serpentinized harzburgite, regular mes."	
"399"	"U1601"	"C"	"122"	"R"	"4"	""	"399-U1601C-122R-4"	"0.0"	"140.0"	"608.970"	"609.670"	"610.370"	"608.623"	"609.261"	"609.9"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Dunite with trace spinel containing corona reaction rims from the top to 24 cm. Between 24 and 76 cm is a harzburgite with 15 % orthopyroxene and trace spinel. This harzburgite has a coarse-grained granular gabbroic domain towards its base. Below 76 cm is a highly altered coarse grained gabbro"	"Variably serpentinized harzburgite and dunite; the harzburgite is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, and chlorite. Highly altered gabbro, appearing greenish and containing sulfides (67-140 cm). It is cut by chlorite veins. The mesh is black and locally greenish. Bastite is grey, green, and black. Spinel is fresh. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Serpentinized harzburgite, dunite, and large normal sense vertical shear zone between gabbro and serpentinized harzburgite, with protomylonitic gabbro overprinted by static alteration."	
"399"	"U1601"	"C"	"123"	"R"	"1"	""	"399-U1601C-123R-1"	"0.0"	"150.0"	"609.900"	"610.650"	"611.400"	"609.9"	"610.65"	"611.4"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The top 72 cm is harzburgite with an average of 15 % orthopyroxene. It is impregnated by diffuse gabbronorite in several places. Below 72 cm is mostly altered gabbro with dunite xenoliths that becomes coarser-grained with depth. This same interval has patches of orthopyroxene-bearing dunite."	"Moderately serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of plagioclase, secondary plagioclase, prehnite, and chlorite. Highly altered gabbro, appearing locally greenish and containing sulfides (72-132 cm). It is cut by chlorite and prehnite veins. Serpentinized dunite at the contact with gabbro contains sulfides. Bastite is grey. Abundant domains with relicts olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins."	"Serpentinized harzburgite above deformed gabbro, protomylonite gabbro with static overprint, shear fabric parallel to gabbro-harzburgite contact. Protomylonite cross-cut by green-white veins."	
"399"	"U1601"	"C"	"123"	"R"	"2"	""	"399-U1601C-123R-2"	"0.0"	"145.0"	"611.400"	"612.125"	"612.850"	"611.4"	"612.125"	"612.85"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"This section is mostly coarse grained gabbro with clinopyroxene crystals up to 3 cm in length. Harzburgite is present at the top of the section; dunite at the bottom."	"Variably altered gabbro and highly serpentinized Opx-bearing dunite. The gabbro is more altered towards the contact with the dunite. Near the contact dunite contains carbonate-sulfide veins. Bastite is grey, green, and black. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Spinel is altered to an unknown brownish phase. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and carbonate-sulfide veins."	"Deformed gabbro, protmylonite, static alteration overprint, conacts with harzburgite above and dunite below."	
"399"	"U1601"	"C"	"123"	"R"	"3"	""	"399-U1601C-123R-3"	"0.0"	"89.0"	"612.850"	"613.295"	"613.740"	"612.85"	"613.295"	"613.74"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with c. 10 % orthopyroxene and diffuse impregnations of gabbro down to 63.5 cm. A pervasively altered, originally coarse-grained gabbro makes up most of the rest of the section. This gabbro contains a significant proportions of an unknown Ti-V bearing mineral. This part of the core also has harzburgite domains."	"Moderately serpentinized harzburgite and pyroxenite. Highly altered gabbro containing serpentinized olivine xenocrysts (57-88 cm). It is cut by chlorite and prehnite veins. Bastite is grey. Some domains with relict olivine and orthopyroxene (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the gabbro."	"Strongly porphyroclastic (0deg) serpentinized harzburgite, moderately foliated mesh (40-45deg)."	
"399"	"U1601"	"C"	"124"	"R"	"1"	""	"399-U1601C-124R-1"	"0.0"	"145.5"	"614.700"	"615.428"	"616.155"	"614.7"	"615.428"	"616.155"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Harzburgite with 12 % orthopyroxene down to 132 cm. A medium-grained olivine wherlite makes up the rest of the section."	"Moderately serpentinized Opx-bearing dunite and pyroxenite. Pyroxene in pyroxenite is altered to chlorite and serpentine. The dunite is cut by a hydrothermally altered magmatic vein made of plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is grey, green, and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the pyroxenite."	"Protogranular serpentinized harzburgite with no mesh. Green vein fault surface is cross cut by little white veins and then overprinted by calcite +pyrite vein."	
"399"	"U1601"	"C"	"124"	"R"	"2"	""	"399-U1601C-124R-2"	"0.0"	"149.0"	"616.155"	"616.900"	"617.645"	"616.155"	"616.9"	"617.645"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 13 % orthopyroxene down to 132 cm. a medium-grained granular gabbro 0.5-1cm wide intrudes steeply through the host harzburgite between 11-74 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite. The harzburgite is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is grey, black, and green. The mesh is black and locally greenish. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and picrolite veins. Picrolite veins cut through the magmatic veins. Chrysotile is less abundant in the lower dunitic part of the section."	"Strongly porphyroclastic (0deg) serpentinized harzburgite, regular patchy mesh."	
"399"	"U1601"	"C"	"124"	"R"	"3"	""	"399-U1601C-124R-3"	"0.0"	"70.5"	"617.640"	"617.992"	"618.345"	"617.64"	"617.992"	"618.345"	""	"1, 2, 3, 4, 5, 6"	""	"This section is mostly harzburgite with c, 16 % orthopyroxene. From 57 cm down is a medium grained, granular gabbronorite."	"Highly serpentinized harzburgite and moderately altered gabbro. Bastite is grey, black, and green. Spinel looks fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"Protogranular serpentinized harzburgite, no mesh."	
"399"	"U1601"	"C"	"125"	"R"	"1"	""	"399-U1601C-125R-1"	"0.0"	"150.0"	"619.600"	"620.350"	"621.100"	"619.6"	"620.297"	"620.993"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The first 4 cm is the gabbronorite continuing from the overlying section. The rest of the section is harzburgite with 20% orthopyroxene and trace chromium spinel. The harzburgite is cut by highly altered at c. 100 cm and between 127 and the base of the section."	"Highly serpentinized harzburgite with variable orthopyroxene abundance (lower at the bottom of the section) and moderately altered gabbro. Harzburgite is cut by hydrothermally altered magmatic veins made of amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Bastite is grey, black, and green. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and composite picrolite-carbonate-sulfides veins. The picrolite-carbonate-sulfide veins cut the magmatic veins."	"Protogranular serpentinized harzburgite, no mesh."	
"399"	"U1601"	"C"	"125"	"R"	"2"	""	"399-U1601C-125R-2"	"0.0"	"140.5"	"621.100"	"621.803"	"622.505"	"620.993"	"621.646"	"622.3"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Most of the section is harzburgite with about 13 % orthopyroxene and a trace of chromium spinel. It is cut by gabbroic veins of uncertain mineralogy as a result of alteration at several locations in the top 29 cm. The interval between 29 and 49.5 cm is dunite with about 3% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite with variable orthopyroxene abundance and moderately altered gabbro. The harzburgite is cut by hydrothermally altered magmatic veins made of clinopyroxene (looks locally brownish), amphibole, plagioclase, and chlorite. The clinopyroxene in the gabbro shows a partial brownish stain. The gabbro is cut by prehnite veins. Bastite is grey, green, and black. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and composite picrolite veins. Picrolite cuts the magmatic veins."	"Protogranular serpentinized harzburgite, no mesh, gabbro."	
"399"	"U1601"	"C"	"125"	"R"	"3"	""	"399-U1601C-125R-3"	"0.0"	"142.5"	"622.505"	"623.217"	"623.930"	"622.297"	"622.96"	"623.622"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Most of the section is harzburgite with about 10 % orthopyroxene and a trace of chromium spinel. At several locations between 7 and 85 cm, the harzburgite is cut by medium-grained olivine gabbro veins, where the olivine is likely derived from the harzburgite. The interval between 85.5 and 103 cm is coarse-grain granular oxide gabbro with magnetite clustered at the center. "	"Highly serpentinized harzburgite with variable orthopyroxene abundance and moderately altered gabbro. Gabbro contains disseminated sulfides (92-95 cm). The gabbro is cut by chlorite-oxide and chlorite-prehnite veins. The harzburgite is cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, prehnite, chlorite, and zeolite(?). Veins appear locally reddish-brown, possibly as a result of oxidation. This section locally contains olivine relicts (variable extent of serpentinization). Bastite is mostly black to grey. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and composite picrolite-zeolite(?) veins. The latter cut through the magmatic veins."	"protogran serp harz, with mylonitized gabbro veins, overprinted with red-green alteration and cross-cut by green undeformed veins."	
"399"	"U1601"	"C"	"125"	"R"	"4"	""	"399-U1601C-125R-4"	"0.0"	"84.0"	"623.930"	"624.350"	"624.770"	"623.62"	"624.01"	"624.401"	""	"1, 2, 3, 4"	""	"Most of the section is harzburgite with about 15 % orthopyroxene and a trace of chromium spinel. Centered at 6cm is a gabbronorite vein about 1 cm thick."	"Highly serpentinized harzburgite and Opx-bearing dunite; the dunite is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, and chlorite. Some olivine relicts (variable extent of serpentinization). Bastite is mostly green, grey, and black. Spinel looks fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive chrysotile veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh. magmatic vein with cross cutting white-green veins which are offset along the margin of the magmatic vein"	
"399"	"U1601"	"C"	"126"	"R"	"1"	""	"399-U1601C-126R-1"	"0.0"	"118.0"	"624.400"	"624.990"	"625.580"	"624.4"	"624.99"	"625.58"	""	"1, 2"	""	"Most of the section is harzburgite with about 25 % orthopyroxene and a trace of chromium spinel. Centered at 6cm is a gabbronorite vein about 1 cm thick. At 31 and 46 cm, the harzburgite is cut by 1-mm-wide gabbronorite veins."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Bastite is mostly green and grey. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh, 0deg little white veins, magmatic vein"	
"399"	"U1601"	"C"	"126"	"R"	"2"	""	"399-U1601C-126R-2"	"0.0"	"150.0"	"625.580"	"626.330"	"627.080"	"625.58"	"626.33"	"627.08"	""	"1, 2"	""	"Most of the section is harzburgite with about 25 % orthopyroxene and a trace of chromium spinel. The harzburgite is cut by a 2-mm-wide gabbronorite vein at 2 cm."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of amphibole, prehnite, and chlorite. Bastite is mostly green and grey. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh, 5deg little white veins,"	
"399"	"U1601"	"C"	"126"	"R"	"3"	""	"399-U1601C-126R-3"	"0.0"	"129.0"	"627.080"	"627.725"	"628.370"	"627.08"	"627.725"	"628.37"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Most of the section is harzburgite with about 20 % orthopyroxene and a trace of chromium spinel. The harzburgite transitions to dunite with trace chromium spinel between 36 and 44 cm. The lower harzburgite is cut by a 2.5-mm-wide gabbronorite vein centered at 123 cm. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is green, grey, and black. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh to moderatley foliated mesh (45deg), 0deg little white veins, magmatic vein"	
"399"	"U1601"	"C"	"127"	"R"	"1"	""	"399-U1601C-127R-1"	"0.0"	"99.0"	"629.300"	"629.795"	"630.290"	"629.3"	"629.788"	"630.276"	""	"1, 2, 3, 4"	""	"Most of the section is harzburgite with about 17% orthopyroxene and a trace of chromium spinel. A diffuse and altered medium-grained gabbro vein cuts the harzburgite in the bottommost piece."	"Moderately to highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is green, grey, and black. Spinel looks fresh. Some olivine relict (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh mesh, 5deg little white veins, magmatic vein"	
"399"	"U1601"	"C"	"127"	"R"	"2"	""	"399-U1601C-127R-2"	"0.0"	"144.0"	"630.290"	"631.010"	"631.730"	"630.276"	"630.986"	"631.695"	""	"1, 2, 3, 4, 5, 6"	""	"The section is harzburgite with about 17% orthopyroxene and a trace of chromium spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is green, grey, and black. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite and chrysotile veins. The latter cut through the magmatic veins."	"protogranular to weakly foliated serp harz (5deg), reg mesh, 0-10deg little white veins, magmatic vein"	
"399"	"U1601"	"C"	"127"	"R"	"3"	""	"399-U1601C-127R-3"	"0.0"	"144.0"	"631.730"	"632.450"	"633.170"	"631.695"	"632.404"	"633.114"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Most of the section is harzburgite with about 10% orthopyroxene and a trace of chromium spinel. The harzburgite is cut by cm-scale altered gabbro veins between 46 and 76 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins made of white to light green mineral (serpentine?), clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is mostly grey and black. Some olivine and pyroxene relicts (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and white massive picrolite and chrysotile veins. The latter cut through the magmatic veins."	"protogranular to weakly foliated serp harz (0deg), no mesh, fault with pyrite slicken fibers"	
"399"	"U1601"	"C"	"127"	"R"	"4"	""	"399-U1601C-127R-4"	"0.0"	"100.0"	"633.170"	"633.670"	"634.170"	"633.114"	"633.607"	"634.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Down to 70 cm, the section is harzburgite with about 10% orthopyroxene and a trace of chromium spinel. Below is a medium-grained gabbro that is noteworthy in the black tinting of the edges of clinopyroxene."	"Highly serpentinized Opx-bearing dunite and highly altered gabbro. Gabbro is cut by prehnite and chlorite veins. Dunite is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, and chlorite. Bastite is mostly grey, black, and green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic veins."	"protogranular to weakly foliated serp harz (0deg), weak foliated mesh (0deg), gabbro with fracturing and brecciation, cut by undeformed transparent vein"	
"399"	"U1601"	"C"	"128"	"R"	"1"	""	"399-U1601C-128R-1"	"0.0"	"143.0"	"634.100"	"634.815"	"635.530"	"634.1"	"634.791"	"635.482"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Most of the section is harzburgite with about 10% orthopyroxene. Gabbro cuts and disrupts the harzburgite from 0-24, 37-49, and 82-87 cm."	"Highly to completely serpentinized Opx-bearing dunite and highly altered gabbro (0-23 cm). Dunite is cut by hydrothermally altered magmatic veins made of prehnite, amphibole, and chlorite. Bastite is mostly black. Mesh is black-brown. Spinel is fresh. The extent of serpentinization is variable. Fracture surfaces that are covered by sulfides. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, no mesh, with gabbro-harz intermixed zone and gabbro with weak deformation fabric (cp?) and fractured, overprinted by static alteration"	
"399"	"U1601"	"C"	"128"	"R"	"2"	""	"399-U1601C-128R-2"	"0.0"	"145.0"	"635.530"	"636.255"	"636.980"	"635.482"	"636.183"	"636.884"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Most of the section is harzburgite with about 10% orthopyroxene. Altered gabbros bearing sulfides cut the harzburgite centered at 54, 76, 94 c, and makes up most of the core beneath 124 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, amphibole, and chlorite. Highly altered gabbro (123-145 cm). Gabbro is cut by prehnite-carbonate-sulfide veins and possibly talc-clay (?) veins that form in fractures through the gabbro. Bastite is mostly black and grey. Spinel is fresh. Sulfide-covered fractures on piece ends. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz, reg mesh, grey altered gabbro layer with sheared contact"	
"399"	"U1601"	"C"	"128"	"R"	"3"	""	"399-U1601C-128R-3"	"0.0"	"125.0"	"636.980"	"637.605"	"638.230"	"636.884"	"637.488"	"638.092"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Most of the section is harzburgite with about 10% orthopyroxene. Altered gabbro veins with sulfide cuts the between 0 and 40 cm, 85-88 cm, 100-1-3 cm, and 116 -118 cm.  makes up most of the core beneath 124 cm. Diabase dikes cut the section at 17-20 cm and 90-99 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of prehnite, amphibole, and chlorite. Highly altered gabbro (0-27 cm) containing carbonates and sulfides. The gabbro is cut by prehnite and chlorite veins. Bastite is mostly black. The mesh is bronze and contains sulfides and carbonate at the contact with the gabbro. Spinel is fresh. Sulfide-covered fractures. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through the magmatic veins."	"serp harz and gabbro intervals, with mylonitic deformation in gabbro and mylonitic deformation in serp harz, parallel to intrusive contacts. Green-grey veins parallel to contacts also sheared with brecciated clasts within. sheared veins are cut by carbonate veins (fizz) and by green veins. Some carbonate veins are faulted with carbonate + chalcopyrite slickenfibers. Late stage overprint of some veins with chalcopyrite is observed, possibly deformed. Minor diabase intervals are unaltered and have intrusive contacts with gabbro and undeformed."	
"399"	"U1601"	"C"	"128"	"R"	"4"	""	"399-U1601C-128R-4"	"0.0"	"94.0"	"638.230"	"638.700"	"639.170"	"638.092"	"638.546"	"639"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This section is harzburgite with about 10% orthopyroxene."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of plagioclase, clinopyroxene, secondary plagioclase, and chlorite. Bastite is mostly black, grey, and green. Spinel is fresh. Sulfide-covered fractures in serpentinites. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through the magmatic veins."	"strongly cp foliated (20deg) serp harz (late deformation) above protogranular serp harz, with moderate mesh foliation (20deg)"	
"399"	"U1601"	"C"	"129"	"R"	"1"	""	"399-U1601C-129R-1"	"0.0"	"150.0"	"639.000"	"639.750"	"640.500"	"639"	"639.75"	"640.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Dunite with chromium spinel trails down to 63 cm. Below is ductilely deformed, coarse grained sulfide-rich gabbro. Sulfides look as though they have pseudomorphed a mafic phase. Some Fe-oxides area also present."	"Highly serpentinized Opx-bearing dunite and highly altered gabbro. Carbonate and sulfide mineralization in the gabbro. Sulfide possibly forms after olivine (in pseudomorphic mesh?). Gabbro is cut by chlorite and prehnite-light green mineral veins. Dunite is cut by hydrothermally altered veins of possible magmatic origin made of chlorite. Bastite is mostly black. Mesh is brown-black. Sulfide-covered fractures in serpentinite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, chlorite, and carbonate-sulfide veins."	"protogranular harz and dunite (moderately foliated) above strongly altered gabbro with protomylonitic fabric and cross cutting brittle faults."	
"399"	"U1601"	"C"	"129"	"R"	"2"	""	"399-U1601C-129R-2"	"0.0"	"150.0"	"640.500"	"641.250"	"642.000"	"640.5"	"641.25"	"642"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Continued ductilely deformed, coarse grained sulfide-rich and oxide-bearing gabbro for the upper 23 cm. Most of the rest of the section is harzburgite with about 12% orthopyroxene and a trace of chromium spinel. A diffuse impregnation of the harzburgite by gabbro is present between 95 and 114 cm."	"Highly serpentinized Opx-bearing dunite and highly altered gabbro (0-21 cm). The gabbro is cut by prehnite and chlorite veins. Dunite is cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, amphibole, prehnite, and chlorite. Bastite is mostly black. Mesh is brown-black. Sulfide-covered fractures in serpentinite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through the magmatic veins."	"altered, fractured gabbro above protogranular to weak foliated serp harz, above late protomylonitic deformation of serp harz"	
"399"	"U1601"	"C"	"129"	"R"	"3"	""	"399-U1601C-129R-3"	"0.0"	"123.0"	"642.000"	"642.615"	"643.230"	"642"	"642.615"	"643.23"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Most of the section is dark harzburgite with about 12% orthopyroxene and a trace of chromium spinel. A coarse-grained gabbro cuts the section from 28-63 cm. Diffuse gabbroic impregnations of the harzburgite are found between 98 and 107 cm."	"Highly to completely serpentinized Opx-bearing dunite and harzburgite. Variably altered and deformed gabbro (27-75 cm). Gabbro is more deformed at the contact with the dunite. The gabbro is cut by talc veins. The serpentinites are cut by hydrothermally altered magmatic veins made of amphibole, prehnite, and chlorite. Bastite is mostly black. Mesh is brown-black. The extent of serpentinization is variable. The last piece is relatively fresh. Spinel looks fresh. Sulfides covered fractures in serpentinite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and massive picrolite veins. The latter cut through the magmatic veins."	"Harz above gabbro above harz. Both gabbro-harz contacts are mylonitized. Mylonitic deformation in both gabbro and harz. Gabbro mylonites deform altered matrix (talc?). Mylonite is cut by talc veins. Top contact mylonite is cut by undeformed thin magmatic vein."	
"399"	"U1601"	"C"	"130"	"R"	"1"	""	"399-U1601C-130R-1"	"0.0"	"140.0"	"643.800"	"644.500"	"645.200"	"643.8"	"644.485"	"645.169"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Most of the section is harzburgite with about 10% orthopyroxene and a trace of chromium spinel. Several dunite intervals bearing about 1% chromium spinel are present. Altered and deformed gabbroic veins cut the peridotites at several places at 46 cm and above. More gabbroic veins are centered at 80, 112, 131, and 142 cm."	"Highly to completely serpentinized harzburgite cut by hydrothermally altered magmatic veins with distinct extents of alteration. They are made of amphibole, prehnite, chlorite, and possibly epidote to plagioclase, amphibole, secondary plagioclase, chlorite, red mineral, and prehnite. Bastite is mostly black. Mesh is brown-black and unusually hard (hardness  3- 4). The extent of serpentinization is variable. Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, sulfide-magnetite veins, and massive picrolite veins. The latter cut through the magmatic veins."	"serp harz with mylonitized gabbro intervals. mylonite is syn- or post-alteration, but then there is a late post-mylonite alteratrion replacing fsp clasts with prehnite spheres."	
"399"	"U1601"	"C"	"130"	"R"	"2"	""	"399-U1601C-130R-2"	"0.0"	"121.0"	"645.200"	"645.805"	"646.410"	"645.169"	"645.76"	"646.352"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Most of the section is harzburgite with about 12% orthopyroxene and a trace of chromium spinel. Patchy gabbroic domains are present at 0-11, 21-27, and 69-74 cm. Diffuse wherlite veins are present between 99.5 and 104 cm."	"Highly to completely serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins displaying variable alteration. They are made of clinopyroxene, plagioclase, amphibole, prehnite, chlorite, and secondary plagioclase. Two types of magmatic veins, one is plastically deformed and another is isotropic. Dunite at the contact is deformed in minor extent. The magmatic veins are crosscut by chlorite, prehnite, and amphibole veins. Bastite is mostly black and then grey and green. Mesh is brown-black, and unusually hard (hardness greater than 3, below 4). Spinel looks fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, sulfide-magnetite veins, and massive picrolite veins. The latter cut through the magmatic veins."	"serp harz with gabbro mylonite and magmatic vein myloniite."	
"399"	"U1601"	"C"	"130"	"R"	"3"	""	"399-U1601C-130R-3"	"0.0"	"140.0"	"646.420"	"647.120"	"647.820"	"646.362"	"647.048"	"647.733"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Most of the section is harzburgite with about 15% orthopyroxene and a trace of chromium spinel down to 74 cm. Coarse grained gabbro completes the section."	"Highly to completely serpentinized harzburgite and variably altered gabbro (74-140 cm). The gabbro is cut by chlorite, amphibole, prehnite, and zeolite veins. The harzburgite is cut by hydrothermally altered magmatic veins. They are made of clinopyroxene, plagioclase, amphibole, prehnite, chlorite, and secondary plagioclase. Bastite is mostly black and minor grey. Mesh is brown-black, and unusually hard (hardness 3-4). Spinel looks fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, sulfide-magnetite veins, and massive picrolite veins. The latter cut through the magmatic veins."	"foliated (late deformatrion) serp harz above gabbro with small sheared interval at base."	
"399"	"U1601"	"C"	"130"	"R"	"4"	""	"399-U1601C-130R-4"	"0.0"	"99.0"	"647.820"	"648.315"	"648.810"	"647.732"	"648.216"	"648.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Coarse-grained poikilitic gabbro."	"Partially deformed and variably altered gabbro locally showing greenschist type alteration. Gabbro is crosscut by chlorite and amphibole veins."	"gabbro with ultramylonite, mylonite, protomylonite, and isotropic sections."	
"399"	"U1601"	"C"	"131"	"R"	"1"	""	"399-U1601C-131R-1"	"0.0"	"142.0"	"648.700"	"649.410"	"650.120"	"648.7"	"649.41"	"650.12"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Medium-grained, poikilitic olivine gabbro with cpx oikocrysts up to 60 mm. Olivine proportion decreases downward towards the olivine-bearing gabbro, which makes up the lower 47 cm of the section."	"Partially deformed and slightly altered gabbro locally showing greenschist-type alteration at the bottom of the section. Gabbro is crosscut by chlorite-prehnite-carbonate, zeolite, and amphibole veins. Some amphibole veins locally contain sulfides."	"gabbro cut by steep mylonite to ultramylonite shear zone with normal sense motion."	
"399"	"U1601"	"C"	"131"	"R"	"2"	""	"399-U1601C-131R-2"	"0.0"	"150.0"	"650.120"	"650.870"	"651.620"	"650.12"	"650.87"	"651.62"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This is an entirely gabbroic section. The top 17-cm continues the olivine-bearing gabbro from the overlying core. The rest is a mix of granular to poikilitic coarse-grained gabbros. An exception is a fine-grained mylonitic oxide gabbro between 103 and 108 cm."	"Partially deformed and moderately altered gabbro. Gabbro is crosscut by chlorite, zeolite, and amphibole veins."	"gabbro with mylonite to protomyloniite sections 30-60deg."	
"399"	"U1601"	"C"	"131"	"R"	"3"	""	"399-U1601C-131R-3"	"0.0"	"144.0"	"651.620"	"652.340"	"653.060"	"651.62"	"652.34"	"653.06"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Coarse-grained and predominantly granular as well as poikilitic gabbro, with textures varying on the 10 m scale."	"Slightly to moderately altered gabbro. Gabbro is crosscut by zeolite and amphibole veins."	"altered gabbro with thin mylonitic intervals"	
"399"	"U1601"	"C"	"132"	"R"	"1"	""	"399-U1601C-132R-1"	"0.0"	"141.0"	"653.500"	"654.205"	"654.910"	"653.5"	"654.205"	"654.91"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Medium to coarse-grained gabbro. The interval between 90-111 cm is diorite with large plagioclase crystals in a matrix containing amphibole and fine-grained metallic minerals with acicular textures. The pXRF showed the matrix to be Fe and Ti rich. "	"Slightly to moderately altered gabbro. Gabbro is crosscut by chlorite, zeolite, and amphibole veins."	"isotropic altered gabbro with protomylonitic intervals. black and white spotty rock with moderately dipping SPO."	
"399"	"U1601"	"C"	"132"	"R"	"2"	""	"399-U1601C-132R-2"	"0.0"	"106.0"	"654.910"	"655.440"	"655.970"	"654.91"	"655.44"	"655.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Coarse-grained and granular gabbro grading downward at 69 cm to a medium-grained and subophitic olivine gabbro."	"Slightly altered gabbro cut by amphibole, chlorite, talc, and zeolite veins."	"isotropic gabbro with grain size variation and cp foliation"	
"399"	"U1601"	"C"	"132"	"R"	"3"	""	"399-U1601C-132R-3"	"0.0"	"92.0"	"655.970"	"656.430"	"656.890"	"655.97"	"656.43"	"656.89"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Medium-grained subophitic olivine-bearing gabbro."	"Slightly to moderately altered gabbro cut by amphibole, chlorite, prehnite, and zeolite veins."	"isotropic gabbro with grain size variation"	
"399"	"U1601"	"C"	"133"	"R"	"1"	""	"399-U1601C-133R-1"	"0.0"	"130.0"	"658.400"	"659.050"	"659.700"	"658.4"	"659.05"	"659.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The upper 62.5 cm is a continuation of the olivine-bearing gabbro from the overlying section. It is underlain by harzburgite with minimal orthopyroxene. This harzburgite is infused with 2-3 cm wide altered gabbroic veins centered at c. 66 and 112 cm."	"Highly serpentinized harzburgite and dunite (0-3 cm; likely fallen piece). The gabbro is cut by chlorite, amphibole, and prehnite veins. The harzburgite is cut by hydrothermally altered magmatic veins made of amphibole, plagioclase, secondary plagioclase, and chlorite. Slightly to moderately altered gabbro (3-62 cm). Mesh appears black. Bastite is grey, black, and green. Spinel is variably altered. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic veins."	"gabbro with ultramylonite band above foliated serp harz"	
"399"	"U1601"	"C"	"133"	"R"	"2"	""	"399-U1601C-133R-2"	"0.0"	"110.0"	"659.700"	"660.250"	"660.800"	"659.7"	"660.25"	"660.8"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with about 12% orthopyroxene. It is cut by a 2-3 cm-wide gabbro vein centered at 69 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears black. Bastite is grey, black, and green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"weakly foliated, shallow, mantle fabric in serp harz, no mesh, mylonite gabbro vein"	
"399"	"U1601"	"C"	"134"	"R"	"1"	""	"399-U1601C-134R-1"	"0.0"	"144.0"	"663.200"	"663.920"	"664.640"	"663.2"	"663.92"	"664.64"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Medium-grained granular gabbro with olivine patches at 43-48 cm and 57-59 cm."	"Moderately altered Ol-bearing gabbro and highly serpentinized dunite at the bottom of the section (139-143 cm). Olivine in the gabbro is partially altered to serpentine and magnetite, or sulfide and serpentine. Sulfide patches occur in gabbro after olivine or orthopyroxene, or both (similar to in 129R, but less mineralized). The gabbro is cut by talc, talc-carbonate, and chlorite-amphibole veins. Mesh appears black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and serpentine-carbonate-sulfide veins."	"altered gabbro with mylonite intervals. talc veins, some cut parallel to mylonite fabric."	
"399"	"U1601"	"C"	"134"	"R"	"2"	""	"399-U1601C-134R-2"	"0.0"	"150.0"	"664.640"	"665.390"	"666.140"	"664.64"	"665.39"	"666.14"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Harzburgite with minimal orthopyroxene and dunite, both with trace chromium spinel. The dunite domain above 51 cm also appears to have trace infused plagioclase, and is cut by highly altered veins of medium-grained granular gabbro. The interval between 51 and 78 cm consists of highly altered and deformed gabbro. Dunite with trace orthopyroxene and chromium spinel makes up the interval between 78 and 95 cm. The lowermost 55 cm is medium-grained granular gabbro, that is mylonitized between 95.5 and 132cm."	"Highly serpentinized Opx-bearing dunite and highly deformed and altered gabbro (56-78 cm and 95-150 cm). The gabbro is cut by amphibole, chlorite, zeolite, and prehnite-carbonate veins. The dunite is cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears black. Bastite is grey and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"gabbro and serp harz with mylonite and ultramylonite gabbro intervals with a crosscutting diabase. "	
"399"	"U1601"	"C"	"134"	"R"	"3"	""	"399-U1601C-134R-3"	"0.0"	"107.0"	"666.140"	"666.675"	"667.210"	"666.14"	"666.675"	"667.21"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The intervals 0-22 and 58-107 cm are medium grained granular gabbros. The interval between 24 and 58 cm is harzburgite with 12% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite and completely serpentinized dunite. Highly altered gabbro (0-24 cm; 71-77 cm and 83-107 cm). The gabbro is cut by prehnite-carbonate veins. Mesh appears black. Bastite is black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"altered gabbro and foliated serp harz and dunite."	
"399"	"U1601"	"C"	"135"	"R"	"1"	""	"399-U1601C-135R-1"	"0.0"	"143.0"	"668.100"	"668.815"	"669.530"	"668.1"	"668.801"	"669.501"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"Coarse- grained granular gabbro continued from the overlying section."	"Highly altered gabbro cut by chlorite, prehnite-carbonate, and zeolite veins."	"altered gabbro, fractured, cut by white veins."	
"399"	"U1601"	"C"	"135"	"R"	"2"	""	"399-U1601C-135R-2"	"0.0"	"126.0"	"669.530"	"670.160"	"670.790"	"669.501"	"670.118"	"670.735"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Coarse- grained granular gabbro continued from the overlying section."	"Highly altered gabbro cut by chlorite, prehnite-carbonate, talc, and zeolite veins."	"altered gabbro, isotropic, minor fracturing, cut by white veins with fault planes."	
"399"	"U1601"	"C"	"135"	"R"	"3"	""	"399-U1601C-135R-3"	"0.0"	"119.0"	"670.790"	"671.385"	"671.980"	"670.735"	"671.318"	"671.901"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Coarse- grained granular gabbro continued from the overlying section from 0 to 19 cm. The rest of the section is harzburgite with minimal orthopyroxene and dunite. Granular and interstitial orthopyroxene is evident."	"Highly serpentinized harzburgite and highly altered gabbro (0-24 cm). Gabbro is cut by prehnite-carbonate veins. Mesh appears black to dark green. Bastite is green to locally reddish. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, serpentine-carbonate veins, and massive picrolite veins."	"protogranular serpentinized harzburgite, regular mesh, with dunite, altered gabbro inerval, protomylonite, deformed talc matrix suggests mylonitization after or during alteration."	
"399"	"U1601"	"C"	"135"	"R"	"4"	""	"399-U1601C-135R-4"	"0.0"	"102.0"	"671.980"	"672.490"	"673.000"	"671.901"	"672.4"	"672.9"	""	"1"	""	"Most of this section is harzburgite with 15% orthopyroxene showing granular and interstitial textures. An orthopyroxene-bearing dunite forms a domain in the upper 26 cm. A 5mm-wide gabbro vein cuts the core at 73 cm."	"Highly serpentinized harzburgite and dunite cut by hydrothermally altered magmatic veins composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears black, grey, and black. Bastite is green, grey, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"porphyroclastic serpentinized harzburgite (70deg), regular mesh, dunite interval"	
"399"	"U1601"	"C"	"136"	"R"	"1"	""	"399-U1601C-136R-1"	"0.0"	"69.0"	"672.900"	"673.245"	"673.590"	"672.9"	"673.245"	"673.59"	""	"1, 2, 3, 4, 5, 6"	""	"Most of this section is orthopyroxene-bearing dunite with trace chromium spinel.  A vein of medium-grained granular gabbro cuts the section at c. 26 cm."	"Highly to completely serpentinized Opx-bearing dunite cut by one hydrothermally altered magmatic vein. The latter is made of amphibole, secondary plagioclase, prehnite, and chlorite. Mesh appears green, white, and black. Bastite is green. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins"	"dunite with reg to moderate foliated mesh (0-30deg)"	
"399"	"U1601"	"C"	"136"	"R"	"2"	""	"399-U1601C-136R-2"	"0.0"	"150.0"	"673.590"	"674.340"	"675.090"	"673.59"	"674.34"	"675.09"	""	"1"	""	"From 0-67 cm are dunite and harzburgite domains, both with trace chromium spinel. Harzburgite with 15% orthopyroxene and trace spinel is below."	"Highly to completely serpentinized harzburgite and dunite cut by one hydrothermally altered magmatic vein. The latter is made of amphibole, secondary plagioclase, and chlorite. Mesh appears green, white, and black. Bastite is green and grey. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins"	"protogranular serp harz with dunite, weak foliated mesh (20deg)"	
"399"	"U1601"	"C"	"136"	"R"	"3"	""	"399-U1601C-136R-3"	"0.0"	"137.0"	"675.090"	"675.775"	"676.460"	"675.09"	"675.775"	"676.46"	""	"1, 2"	""	"Most of the section is harzburgite with 13% orthopyroxene and trace spinel. A medium grained granular gabbro cuts the section between 104 and 107 cm. Orthopyroxene-bearing dunite completes the section."	"Highly to completely serpentinized harzburgite and dunite (at the bottom of the section; 100-137 cm) cut by hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Mesh appears green and black. Bastite is green and grey. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chysotile veins."	"strong porphyrolcastic (STEEP 70deg) serp harz, dunite interval, weak to reg mesh (10deg) cut by gently dipping magmatic vein."	
"399"	"U1601"	"C"	"136"	"R"	"4"	""	"399-U1601C-136R-4"	"0.0"	"113.0"	"676.460"	"677.025"	"677.590"	"676.46"	"677.025"	"677.59"	""	"1, 2"	""	"Most of the section is harzburgite with 13% orthopyroxene and trace spinel. Dunite makes up the interval: 80-88 cm."	"Highly serpentinized harzburgite and dunite. Mesh appears grey and black. Bastite is green, grey, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins. Some chrysotile veins are thicker (up to 3 mm) than those forming the network (0.2 mm)."	"strong porphyrolcastic (STEEP 70deg) serp harz, irregular pactchy zones of dunite, reg to mod mesh (70deg)."	
"399"	"U1601"	"C"	"137"	"R"	"1"	""	"399-U1601C-137R-1"	"0.0"	"139.0"	"677.800"	"678.495"	"679.190"	"677.8"	"678.495"	"679.19"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 13% orthopyroxene, trace clinopyroxene, and trace chromium spinel. Most of the orthopyroxene is of the granular variety."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of plagioclase and a brown-reddish material (clays after clinopyroxene?). Mesh appears grey and black. Bastite is green, grey, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz and dunite with weak foliated mesh (30deg)"	
"399"	"U1601"	"C"	"137"	"R"	"2"	""	"399-U1601C-137R-2"	"0.0"	"117.0"	"679.190"	"679.775"	"680.360"	"679.19"	"679.775"	"680.36"	""	"1, 2, 3, 4"	""	"Mostly harzburgite with 13% orthopyroxene, trace clinopyroxene, and trace chromium spinel. Most of the orthopyroxene is of the granular variety. A 3-cm wide gabbro vein cuts the section from 29 to 32 cm."	"Highly serpentinized harzburgite and dunite; the latter is cut by one hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears grey and black. Bastite is green, grey, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz with reg mesh cut by sub-horizontal magmatic vein."	
"399"	"U1601"	"C"	"137"	"R"	"3"	""	"399-U1601C-137R-3"	"0.0"	"101.0"	"680.360"	"680.865"	"681.370"	"680.36"	"680.865"	"681.37"	""	"1, 2, 3, 4"	""	"Harzburgite with 10% orthopyroxene and trace chromium spinel. Most of the orthopyroxene is of the granular variety."	"Highly serpentinized harzburgite and Opx-bearing dunite cut by hydrothermally altered magmatic veins made of clinopyroxene (brown alteration), amphibole, secondary plagioclase, and chlorite. Mesh appears grey and black. It is locally brownish. Bastite is green, grey, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz with reg mesh"	
"399"	"U1601"	"C"	"137"	"R"	"4"	""	"399-U1601C-137R-4"	"0.0"	"93.0"	"681.370"	"681.835"	"682.300"	"681.37"	"681.835"	"682.3"	""	"1, 2, 3, 4, 5, 6"	""	"Mostly harzburgite with 15% orthopyroxene and trace chromium spinel. Most of the orthopyroxene is of the granular variety. A short interval of highly altered gabbro cuts the section between 6.5 and 13.5 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, prehnite, carbonates, chlorite, and amphibole. Mesh appears green, black, and grey. It is locally brownish. Bastite is green and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins. The magmatic vein is cut by prehnite-carbonate veins."	"porphyrolcastic mantle fabric (STEEP 85deg) serp harz, reg mesh"	
"399"	"U1601"	"C"	"138"	"R"	"1"	""	"399-U1601C-138R-1"	"0.0"	"150.0"	"682.600"	"683.350"	"684.100"	"682.6"	"683.322"	"684.044"	""	"1, 2, 3, 4, 5"	""	"Harzburgite with 15% orthopyroxene and trace chromium spinel. "	"Moderately to highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, prehnite, and secondary plagioclase. Mesh appears black and grey. Bastite is green, grey, and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"porphyrolcastic (VERTICAL 90deg) serp harz, reg to weak mesh (15deg)"	
"399"	"U1601"	"C"	"138"	"R"	"2"	""	"399-U1601C-138R-2"	"0.0"	"137.0"	"684.100"	"684.785"	"685.470"	"684.044"	"684.703"	"685.363"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Dunite with trace chromium spinel through the first 5 cm followed by a coarse-grained granular gabbro down to 28 cm. The interval from 28 to 87 cm is harzburgite with 10% orthopyroxene and trace chromium spinel. Below 87 cm and to the bottom of the section is coarse-grained, granular to subophitic gabbro."	"Variably altered gabbro and highly serpentinized harzburgite. The gabbro is cut by chlorite and prehnite-carbonate veins. Mesh appears black. Bastite is grey and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and sulfide veins."	"protogranular serp harz, no mesh, gabbro intervals, talc-altered protmylonite conact, with deformed talc."	
"399"	"U1601"	"C"	"138"	"R"	"3"	""	"399-U1601C-138R-3"	"0.0"	"150.0"	"685.470"	"686.220"	"686.970"	"685.363"	"686.085"	"686.807"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"The coarse-grained, granular to subophitic gabbro continues from the overlying section down to135.5 cm. It is underlain by dunite with trace chromium spinel."	"Variably altered gabbro, fresh in the upper part of the section. It is cut by amphibole, chlorite, talc-carbonate, and zeolite veins. Highly serpentinized dunite at the bottom of the section (134-149 cm). The latter is cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, secondary plagioclase, prehnite, and chlorite. Mesh appears black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"altered gabbro, isotropic, with grain size variations, fractured, cut by talc veins"	
"399"	"U1601"	"C"	"138"	"R"	"4"	""	"399-U1601C-138R-4"	"0.0"	"72.0"	"686.970"	"687.330"	"687.690"	"686.807"	"687.154"	"687.5"	""	"1, 2, 3, 4, 5"	""	"The dunite from the overlying section continues down to 17 cm. It is underlain by harzburgite with 10% orthopyroxene."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of amphibole and chlorite. Mesh appears dark green to black. Bastite is green to red. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins"	"protogranular serp harz and dunite with reg to weak fol mesh (10deg)"	
"399"	"U1601"	"C"	"139"	"R"	"1"	""	"399-U1601C-139R-1"	"0.0"	"140.0"	"687.500"	"688.200"	"688.900"	"687.5"	"688.2"	"688.9"	""	"1, 2, 3, 4, 5"	""	"The uppermost 58 cm is orthopyroxene-bearing dunite with trace spinel. A coarse-grained gabbro is present near thecontact with opx-bearing dunite. Below is a medium-grained olivine gabbro. 2 cm of coarse-grained gabbro reappears at 120 cm."	"Variably altered gabbro and highly serpentinized Opx-bearing dunite. The gabbro is cut by hydrothermally overprinted magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, amphibole, and chlorite. Besides, chlorite, talc-carbonate-sulfide, and zeolite veins cut through the gabbro. Mesh appears grey, black, and green. Bastite is green to black. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins"	"dunite above altered gabbro with mingled serp harz"	
"399"	"U1601"	"C"	"139"	"R"	"2"	""	"399-U1601C-139R-2"	"0.0"	"133.0"	"688.900"	"689.565"	"690.230"	"688.9"	"689.565"	"690.23"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Most of this section is medium to coarse-grained olivine gabbro, with sulfides noted below 94 cm. Highly altered harzburgite, originally with c. 10% orhtopyroxene is located between 53 and 94 cm."	"Variably altered gabbro and highly serpentinized hazrburgite. The gabbro is cut by talc-light green mineral-carbonate-sulfide veins and amphibole veins. Mesh appears greenish. Bastite is black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and sulfide veins."	"altered very fine grained gabbro and protogranular serp harz, weak mesh fol (30deg)"	
"399"	"U1601"	"C"	"139"	"R"	"3"	""	"399-U1601C-139R-3"	"0.0"	"89.0"	"690.230"	"690.675"	"691.120"	"690.23"	"690.675"	"691.12"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Mostly harzburgite with c, 10% orthopyroxene. Highly altered coarse-grained gabbro cuts the section between 50 and 73 cm."	"Highly serpentinized and mineralized harzburgite and variably altered gabbro. The gabbro is cut by chlorite and talc veins. Mesh appears greenish to grey to black. Bastite is black. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, massive picrolite veins, thick talc-amphibole-chlorite-carbonate-sulfides veins (25 mm), and sulfide veins."	"light grey altered serp harz protogranular weak (45deg) to no mesh, altered gabbro."	
"399"	"U1601"	"C"	"140"	"R"	"1"	""	"399-U1601C-140R-1"	"0.0"	"141.0"	"692.300"	"693.005"	"693.710"	"692.3"	"693.005"	"693.71"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This core contains a nearly vertical contact between a gabbroic intrusion and dunite running nearly the entire length of the section. The dunite contains trace to 1% chromium spinel. The gabbro is medium to coarse grained and granular."	"Highly serpentinized Opx-bearing dunite and variably altered gabbro (21-117 cm). The gabbro is cut by amphibole, talc-carbonate, and zeolite veins. At the contact with gabbro, dunite is mineralized and does not contain orthopyroxene, and displays a brownish color. Close to the contact gabbro shows reddish color (possibly clays after clinopyroxene?). Mesh appears brown to black and contains sulfides. Bastite is black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and sulfides veins."	"dunite with weak serp foliation (40-10deg), with altered coarse grained gabbro interval, with steep contacts."	
"399"	"U1601"	"C"	"140"	"R"	"2"	""	"399-U1601C-140R-2"	"0.0"	"128.0"	"693.710"	"694.350"	"694.990"	"693.71"	"694.35"	"694.99"	""	"1, 2, 3, 4, 5, 6"	""	"Most of this section is dunite with trace chromium spinel. A medium-grained granular gabbro domain is present between 5 and 17 cm. This gabbro is a continuation of the gabbro within the overlying section."	"Highly serpentinized dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, talc (light-green), and clay minerals. Mesh appears greenish. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and sulfides veins that are oxidized."	"dunite with weak foliated mesh (10deg), sheared gabbro contact."	
"399"	"U1601"	"C"	"140"	"R"	"3"	""	"399-U1601C-140R-3"	"0.0"	"121.0"	"694.990"	"695.595"	"696.200"	"694.99"	"695.595"	"696.2"	""	"1, 2, 3, 4"	""	"Dunite with trace chromium spinel atop harzburgite with 10% orthopyroxene."	"Highly serpentinized Opx-bearing and Opx-free dunite cut by hydrothermally altered magmatic veins made of brownish clinopyroxene (clays?), amphibole, secondary plagioclase, and chlorite? Mesh appears black and greenish. Bastite is grey to black. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and massive picrolite veins. The latter cut through magmatic veins"	"dunite and protogranular serp harz with weak foliated mesh (20deg) to no mesh. large vertical green vein with normal offset"	
"399"	"U1601"	"C"	"140"	"R"	"4"	""	"399-U1601C-140R-4"	"0.0"	"59.0"	"696.200"	"696.495"	"696.790"	"696.2"	"696.495"	"696.79"	""	"1, 2, 3"	""	"Harzburgite with 10% orthopyroxene continued."	"Highly serpentinized harzburgite. Mesh appears black. Bastite is grey to black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and oxidized sulfide veins."	"protogranular serp harz, reg mesh"	
"399"	"U1601"	"C"	"141"	"R"	"1"	""	"399-U1601C-141R-1"	"0.0"	"101.0"	"697.200"	"697.705"	"698.210"	"697.2"	"697.705"	"698.21"	""	"1, 2, 3, 4"	""	"Most of this section is harzburgite with 12% orthopyroxene and trace spinel. Coaarse-grained granular gabbro veins are found between 82 and 84 cm and below 97 cm. Dunite with c. 1% chromium spinel crosses the section from 89 to 97 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Moderately altered gabbro cut by chlorite and zeolite veins. Mesh appears black. Bastite is grey to black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg mesh, magmatic veins (mod dipping) with green white veins."	
"399"	"U1601"	"C"	"141"	"R"	"2"	""	"399-U1601C-141R-2"	"0.0"	"54.0"	"698.210"	"698.480"	"698.750"	"698.21"	"698.48"	"698.75"	""	"1, 2, 3, 4, 5, 6"	""	"Highly altered medium-grained granular gabbro, which has a mylonite zone from 42to 50cm."	"Highly altered and deformed gabbro cut by chlorite and zeolite veins."	"unoriented peices of gabbro, fractured and with a mylonite."	
"399"	"U1601"	"C"	"142"	"R"	"1"	""	"399-U1601C-142R-1"	"0.0"	"150.0"	"702.000"	"702.750"	"703.500"	"702"	"702.75"	"703.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Harzburgite with 10 % orthopyroxene and trace chromium spinel cut by an aphanitic diabase with serpentinized mantle xenoliths."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Variably altered microgabbro cut by carbonate-prehnite-chlorite-sulfide veins. Mesh appears black to brown. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite to white serpentine veins. The latter cut through magmatic veins."	"serp harz, undetermined fabric due to veining. magmatic veins, cut by green-white veins, cut by little white veins. above altered fractured diabase with white calcite veins filling fracture network."	
"399"	"U1601"	"C"	"142"	"R"	"2"	""	"399-U1601C-142R-2"	"0.0"	"150.0"	"703.500"	"704.250"	"705.000"	"703.5"	"704.25"	"705"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with with 13% orthopyroxene and trace chromium spinel makes up most of the section. It is cut by a highly altered gabbroic vein between 119 and 123 cm."	"Highly serpentinized harzburgite / Opx-bearing dunite. Dunite is cut by a hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Mesh appears black to brown. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg to strong fol mesh (65deg) with rubble at the top."	
"399"	"U1601"	"C"	"142"	"R"	"3"	""	"399-U1601C-142R-3"	"0.0"	"117.0"	"705.000"	"705.585"	"706.170"	"705"	"705.585"	"706.17"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Harzburgite with with 13% orthopyroxene and trace chromium spinel makes up most of the section. Highly altered gabbroic veins cut the section centered at 10, 50, 64, 78, and 87  cm."	"Highly serpentinized harzburgite and Opx-bearing dunite; both are cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Mesh appears black to brown. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"serp harz, undetermined fabric due to veining. magmatic veins 1st gen, big white veins 2nd, green/little white veins 3rd generation."	
"399"	"U1601"	"C"	"142"	"R"	"4"	""	"399-U1601C-142R-4"	"0.0"	"66.0"	"706.170"	"706.500"	"706.830"	"706.17"	"706.5"	"706.83"	""	"1, 2, 3, 4"	""	"Harzburgite with 17% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite and minor Opx-bearing dunite; both are cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite. Oxidation of the magmatic vein (brown aspect)? The extent of serpentinization is variable throughout the section. Mesh appears grey to black. Bastite is grey, green, and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg mesh cut by several veins."	
"399"	"U1601"	"C"	"143"	"R"	"1"	""	"399-U1601C-143R-1"	"0.0"	"127.0"	"706.900"	"707.535"	"708.170"	"706.9"	"707.535"	"708.17"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Dunite with trace chromium spinel above 17 cm, underlain by harzburgite with 10% orthopyroxene. Highly altered gabbroic veins 1 to several cm thick cut the section in several places throughout the section. Unusually reddish alteration minerals have replaced portions of the gabbroic veins."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic vein made of plagioclase. The magmatic vein shows a brown stain. Mesh appears grey to black. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, weakly foliated (15deg) mesh, red-green-white steeply dipping magmatic veins cut by white veins."	
"399"	"U1601"	"C"	"143"	"R"	"2"	""	"399-U1601C-143R-2"	"0.0"	"61.0"	"708.170"	"708.475"	"708.780"	"708.17"	"708.475"	"708.78"	""	"1, 2, 3, 4, 5, 6"	""	"Most of the section is orthopyroxene-bearing dunite, with mm-scale altered gabbroic veins cutting the section especially in the upper 21 cm."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, secondary plagioclase, and chlorite. The extent of serpentinization is variable with some relicts of coarse orthopyroxene. Mesh appears black. Bastite is grey and green. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"serp harz "infused" with gabbro, lots of veins, not possible to determine fabrics"	
"399"	"U1601"	"C"	"144"	"R"	"1"	""	"399-U1601C-144R-1"	"0.0"	"145.0"	"711.700"	"712.425"	"713.150"	"711.7"	"712.425"	"713.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Most of the section is orthopyroxene-bearing dunite with trace chromium spinel. Medium grained granular gabbroic veins cut the section at 60 cm and below 100 cm. The deeper ones are highly altered."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein made of plagioclase, amphibole, chlorite, and prehnite. Mesh appears black and grey. Bastite is grey, black, green, and white. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-prehnite-chlorite(?) veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg to weak mesh (60deg), lots of veins"	
"399"	"U1601"	"C"	"144"	"R"	"2"	""	"399-U1601C-144R-2"	"0.0"	"133.0"	"713.150"	"713.815"	"714.480"	"713.15"	"713.815"	"714.48"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is mostly diabase with fine grained to aphanitic textures. Orthopyroxene-bearing dunite wallrocks are scattered through the section."	"Variably altered diabase/microgabbro brecciated with carbonate-prehnite-chlorite-sulfide veins. The microgabbro is cut by zeolite veins. The microgabbro surrounds highly serpentinized Opx-bearing dunite clasts that contain chrysotile and picrolite veins."	"diabase intensly fractured (hydrofractured?) with white vein fill, some fault breccia. unorientaed peice contains diabase-harz contact, which is veined."	
"399"	"U1601"	"C"	"144"	"R"	"3"	""	"399-U1601C-144R-3"	"0.0"	"103.0"	"714.480"	"714.995"	"715.510"	"714.48"	"714.995"	"715.51"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section from 0 to 78 cm is diabase continued from the overlying section. Below is a harzburgite with 10% orthopyroxene and trace spinel."	"Variably altered diabase/microgabbro and highly serpentinized Opx-bearing dunite/harzburgite. Microgabbro has chilled margins. It is cut by carbonate-prehnite-chlorite-sulfide veins and zeolite veins. Mesh is black and grey. Bastite is grey to green. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chysotile veins"	"dibase intensly fractured (hydrofractured?) with white vein fill, some fault breccia, above dunite and serp harz"	
"399"	"U1601"	"C"	"145"	"R"	"1"	""	"399-U1601C-145R-1"	"0.0"	"147.0"	"716.600"	"717.335"	"718.070"	"716.6"	"717.287"	"717.973"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is dominantly harzburgite averaging 13 % orthopyroxene and a trace of chromium spinel. A medium-grained gabbroic vein cuts the section at 101 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, and chlorite. Mesh appears grey to black. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular to porphyroclastic (0deg) serp harz, with reg to SUBVERTICAL moderately fol (30-90deg) mesh."	
"399"	"U1601"	"C"	"145"	"R"	"2"	""	"399-U1601C-145R-2"	"0.0"	"137.0"	"718.070"	"718.755"	"719.440"	"717.973"	"718.612"	"719.252"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Harzburgite with 18% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears grey, green, and black. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular porphyroclastic (10-15deg) serp harz, reg mesh cut by green veins."	
"399"	"U1601"	"C"	"145"	"R"	"3"	""	"399-U1601C-145R-3"	"0.0"	"132.0"	"719.440"	"720.100"	"720.760"	"719.252"	"719.869"	"720.485"	""	"1, 2"	""	"Medium-grained granular gabbro for the topmost 3 cm. From 3 to 9 cm is dunite with trace chromium spinel. Below is harzburgite with c. 15 % orthopyroxene and trace chromium spinel. A nearly vertical gabbroic vein cuts the section between 103 and 123 cm."	"Highly serpentinized harzburgite and dunite (upper part of the section); both are cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears black, grey, and green. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"dunite and protogranular serp harz, reg mesh with rare and thin magmatic veins."	
"399"	"U1601"	"C"	"145"	"R"	"4"	""	"399-U1601C-145R-4"	"0.0"	"98.0"	"720.760"	"721.250"	"721.740"	"720.485"	"720.942"	"721.4"	""	"1, 2"	""	"Most of the section is harzburgite with c. 15 % orthopyroxene and trace chromium spinel. A nearly vertical, thin gabbroic vein cuts through almost the entire length of the section."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh appears black, grey, and green. Bastite is grey, green, and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, patchy reg mesh with magmatic veins."	
"399"	"U1601"	"C"	"146"	"R"	"1"	""	"399-U1601C-146R-1"	"0.0"	"146.0"	"721.400"	"722.130"	"722.860"	"721.4"	"722.13"	"722.86"	""	"1, 2, 3, 4, 5, 6"	""	"Most of the section is harzburgite with c. 15 % orthopyroxene and trace chromium spinel."	"Whole round section. Rock color is black, grey, white, and green. Based on whole round density and magnetic susceptibility measurements, it is estimated that the peridotite is highly serpentinized. This serpentinized Opx-bearing peridotite is cut by numerous white chrysotile veins, less than 1 mm wide. Some of them are forming slickensides on piece ends."	"Protogranular serpentinized harzburgite crosscut by chrysotile veins."	
"399"	"U1601"	"C"	"146"	"R"	"2"	""	"399-U1601C-146R-2"	"0.0"	"140.0"	"722.860"	"723.560"	"724.260"	"722.86"	"723.56"	"724.26"	""	"1, 2, 3, 4, 5, 6"	""	"Most of the section is harzburgite with c. 15 % orthopyroxene and trace chromium spinel."	"Whole round section. Rock color is black, grey, white, and green. Based on whole round density and magnetic susceptibility measurements, it is estimated that the peridotite is highly serpentinized. This serpentinized Opx-bearing peridotite is cut by numerous white chrysotile veins, less than 5 mm wide. Fragmented pieces of serpentinized peridoite are abundant at the end of the section."	"Protogranular to weakly foliated serpentinized harzburgite crosscut by white chrysotile veins."	
"399"	"U1601"	"C"	"146"	"R"	"3"	""	"399-U1601C-146R-3"	"0.0"	"123.0"	"724.260"	"724.875"	"725.490"	"724.26"	"724.875"	"725.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"The top is harzburgite down to 35 cm. Beneath is a medium-grained granular gabbro."	"Whole round section. Rock color is grey, black, white, and green. Based on whole round density and magnetic susceptibility measurements, it is estimated that the top of the section is highly serpentinized peridotite. Much of the section is moderately to highly altered gabbro. The contact between altered gabbro and serpentinized peridotite is whitish. Set of picrolite veins cut through the contact, up to 4 mm. "	"Protogranular serpentinized harzburgite above pegmatitic isotropic gabbro."	
"399"	"U1601"	"C"	"146"	"R"	"4"	""	"399-U1601C-146R-4"	"0.0"	"30.0"	"725.650"	"725.800"	"725.950"	"725.65"	"725.8"	"725.95"	""	"1, 2"	""	"This section is medium grained gabbro"	"Moderately to highly altered gabbro that is cut by rare zeolite veins."	"Coarse grained isotropic gabbro."	
"399"	"U1601"	"C"	"147"	"R"	"1"	""	"399-U1601C-147R-1"	"0.0"	"141.0"	"726.300"	"727.005"	"727.710"	"726.3"	"727.005"	"727.71"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Most of this section is medium to coarse-grained gabbro. Between 80 and 94 cm, the gabbro is highly deformed with reddish plagioclase. Harzburgite with 12% orthopyroxene and trace chromium spinel is in the intervals: 22-33 cm and 94-112 cm. The interstitial variety of orthopyroxene is common."	"Altered gabbro and highly serpentinized harzburgite cut by hydrothermally altered magmatic vein made of brown-stained Cpx, chlorite, and amphibole. Mesh is black, brown, grey, and green. Bastite is green and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite and serpentine-sulfide veins in mesh texture, a network of fibrous to massive chrysotile veins, carbonate-sulfide, and massive picrolite veins. The latter cut through magmatic veins. Amphibole, talc-carbonate veins in gabbro."	"coarse pyroxene pegmatite above serp harz, above pyroxene pegmatite, above gabbro. Then gabbro ultramylonite intruded by gabbro. White magmatic vein intrudes harz to base of mylonite. mylonite and harz is cut by talc veins."	
"399"	"U1601"	"C"	"147"	"R"	"2"	""	"399-U1601C-147R-2"	"0.0"	"147.0"	"727.710"	"728.445"	"729.180"	"727.71"	"728.445"	"729.18"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Most of this section is harzburgite with 20% orthopyroxene and trace chromium spinel. The interstitial variety of orthopyroxene is common. A 1cm-thick gabbro vein cuts the harzburgite centered at 26 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein made of brown-stand Cpx, amphibole, secondary plag, prehnite, and chlorite. Mesh is black and brown and locally grey. Bastite is mostly black and locally green. olivine relicts exist close to bastite. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz above strongly foliated serpentinized harzburgite cut by moderately dipping magmatic vein."	
"399"	"U1601"	"C"	"148"	"R"	"1"	""	"399-U1601C-148R-1"	"0.0"	"139.0"	"731.100"	"731.795"	"732.490"	"731.1"	"731.795"	"732.49"	""	"1, 2, 3, 4, 5, 6"	""	"From 0-35 cm is dunite with trace chromium spinel. The rest of the section is harzburgite  with 17 % orthopyroxene, trace clinopyroxene, and trace chromium spinel."	"Highly serpentinized harzburgite and dunite cut by hydrothermally altered magmatic veins made of amphibole, secondary plagioclase, prehnite, and chlorite. Mesh appears black, grey, and brown. Bastite is green and grey. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz and dunite, reg mesh with magmatic veins."	
"399"	"U1601"	"C"	"148"	"R"	"2"	""	"399-U1601C-148R-2"	"0.0"	"128.0"	"732.490"	"733.130"	"733.770"	"732.49"	"733.13"	"733.77"	""	"1, 2, 3"	""	"The length of the section has harzburgite with c. 20% orthopyroxene and trace clinopyroxene and chromium spinel. This domain is noteworthy in that it contains the largest orthopyroxene grain seen thus far at 3 cm.  A prominent dunite with about 1% chromium spinel makes up much of the section below 74 cm. "	"Highly serpentinized harzburgite and dunite; harzburgite cut by hydrothermally altered magmatic veins made of chlorite, amphibole, and prehnite. Mesh appears black and green. Bastite is green and grey. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and a network of fibrous to massive chrysotile veins."	"protogranular serp harz and dunite, reg to no mesh"	
"399"	"U1601"	"C"	"148"	"R"	"3"	""	"399-U1601C-148R-3"	"0.0"	"145.0"	"733.770"	"734.495"	"735.220"	"733.77"	"734.495"	"735.22"	""	"1, 2, 3, 4, 5, 6"	""	"The dunite from the overlying section continues down to 69 cm. The largest spiinel is about 8mm in length at c. 18 cm. Harzburgite, with 15 % orthopyroxene increasing to 35% down section, underlies the dunite. The orthopyroxene is largely granular here."	"Moderately to highly serpentinized harzburgite and Opx-bearing dunite; the latter is cut by one hydrothermally altered magmatic vein made of chlorite, amphibole, and prehnite. Dunite is at the top of the section. The extent of serpentinization is variable in harzburgite, some areas contain relicts of olivine and Opx (~50% serpentinization). Mesh appears black and green. Bastite is green and grey. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, massive picrolite veins, and carbonate veins."	"dunite and strongly porphyroclastic (0-10deg) serp harz, reg mesh."	
"399"	"U1601"	"C"	"149"	"R"	"1"	""	"399-U1601C-149R-1"	"0.0"	"142.0"	"736.000"	"736.710"	"737.420"	"736"	"736.621"	"737.242"	""	"1, 2, 3, 4, 5, 6"	""	"This section is relatively fresh harzburgite with abundant (c. 35%) granular orthopyroxene, trace clinopyroxene and trace chromium spinel. A 1mm wide gabbroic vein cuts the section at about 116 cm."	"Least altered harzburgite so far: moderately serpentinized harzburgite cut by three hydrothermally altered magmatic veins made of plagioclase, chlorite, amphibole, secondary plagioclase, and prehnite. The extent of serpentinization is variable, and some areas contain up to 70% relics of olivine and Opx. Mesh appears black, grey, and green. Bastite is grey, black, and green; it tends to be black close to magmatic veins. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chysotile veins, and massive picrolite veins."	"protogranular serp harz, with incipient mesh with black veins creating foliation (0-65deg)"	
"399"	"U1601"	"C"	"149"	"R"	"2"	""	"399-U1601C-149R-2"	"0.0"	"116.0"	"737.420"	"738.000"	"738.580"	"737.242"	"737.749"	"738.256"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is relatively fresh harzburgite with abundant (c. 30-35%) granular orthopyroxene, trace clinopyroxene and trace chromium spinel. "	"Variably serpentinized harzburgite cut by three hydrothermally altered magmatic veins made of plagioclase, chlorite, amphibole, secondary plagioclase, and prehnite. Mesh appears black, brown, and grey. Bastite is grey, black, and green. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chysotile veins, and massive picrolite veins."	"porphyroclastic (45deg) serp harz, incipient mesh."	
"399"	"U1601"	"C"	"149"	"R"	"3"	""	"399-U1601C-149R-3"	"0.0"	"142.0"	"738.580"	"739.290"	"740.000"	"738.256"	"738.876"	"739.497"	""	"1, 2"	""	"This section is relatively fresh harzburgite with abundant (c. 30-35%) granular orthopyroxene, trace clinopyroxene and trace chromium spinel. "	"Least altered harzburgite so far: Moderately serpentinized Cpx-bearing harzburgite cut by one hydrothermally altered magmatic vein made of chlorite amphibole, and secondary plagioclase. Mesh appears black, grey, and brown. Bastite is green to grey. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and one fibrous to massive chrysotile vein."	"protogranular serp harz, incipient mesh."	
"399"	"U1601"	"C"	"149"	"R"	"4"	""	"399-U1601C-149R-4"	"0.0"	"149.0"	"740.000"	"740.745"	"741.490"	"739.497"	"740.149"	"740.8"	""	"1, 2, 3"	""	"This section is relatively fresh harzburgite with abundant (c. 30-35%) granular orthopyroxene, trace clinopyroxene and trace chromium spinel. A 2mm wide gabbroic vein cuts the section at about 40 cm."	"Variably serpentinized harzburgite cut by two hydrothermally altered magmatic veins made of plagioclase, secondary plagioclase, amphibole, and chlorite. Mesh appears black, brown, and grey. Bastite is green to grey and black; it is black close to the chlorite-amphibole magmatic vein. The extent of serpentinization increases down section. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, sets of fibrous to massive chrysotile veins, and chlorite veins."	"protogranular serp harz, incipient mesh."	
"399"	"U1601"	"C"	"150"	"R"	"1"	""	"399-U1601C-150R-1"	"0.0"	"133.0"	"740.800"	"741.465"	"742.130"	"740.8"	"741.465"	"742.13"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with 12 % orthopyroxene (both granular and interstitial) and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by one hydrothermally altered magmatic vein made of chlorite, prehnite, and secondary plagioclase. Mesh appears black, brown, and grey. Bastite is green and grey and locally has a black corona. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, sets of fibrous to massive chrysotile veins, and picrolite veins."	"protogranular to porphyroclastic (20-50deg) serp harz, reg mesh and little white veins."	
"399"	"U1601"	"C"	"150"	"R"	"2"	""	"399-U1601C-150R-2"	"0.0"	"151.0"	"742.140"	"742.895"	"743.650"	"742.14"	"742.895"	"743.65"	""	"1, 2, 3"	""	"This section is mostly harzburgite with 14 % orthopyroxene (both granular and interstitial) and trace chromium spinel. A medium grained granular gabbro is in pebbles within the bin between 131 and 144 cm."	"Highly serpentinized harzburgite cut by sets of hydrothermally altered magmatic veins made of chlorite, Cpx, plagioclase, amphibole, prehnite, and secondary plagioclase. Mesh appears black, brown, and grey. Bastite is green, grey, and black. The extent of serpentinization is locally variable. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins."	"protogranular to porphyroclastic (10deg) serp harz, reg to weak fol mesh (10deg) cut by several magmatic veins."	
"399"	"U1601"	"C"	"150"	"R"	"3"	""	"399-U1601C-150R-3"	"0.0"	"151.0"	"743.660"	"744.415"	"745.170"	"743.66"	"744.415"	"745.17"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The top of the section is harzburgite similar to that in the overlying section. Below 91 cm is a granular olivine microgabbro with a few ophitic cpx. Grain sizes gradually increase down section."	"Highly serpentinized Opx-bearing dunite and variably altered microgabbro. In serpentinite, mesh appears black, brown, and grey. Bastite is green, grey, and black. Microgabbro contains amphibole after Cpx and chlorite after plagioclase. Microgabbro becomes coarser-grained down section. The top of the section is locally fresher. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and a massive green vein. The microgabbro contains talc-carbonate veins and prehnite-chlorite-carbonate veins."	"porphyroclastic (20deg) to protogranular serp harz, reg mesh, inturded by undeformed microgabbro, the microgabbro has variable grain size, and the interval includes internal grain size contacts."	
"399"	"U1601"	"C"	"151"	"R"	"1"	""	"399-U1601C-151R-1"	"0.0"	"144.5"	"745.700"	"746.423"	"747.145"	"745.7"	"746.423"	"747.145"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"This section is a medium-grained granular gabbro with variation in crystal size and texture on ~10 cm scale. It is a continuation from the overlying core."	"Variably altered Ol-gabbro. The extent of alteration increases toward hydrothermal veins. Plagioclase is altered to prehnite, chlorite, and secondary plagioclase close to the veins, while it is altered to chlorite far from the veins. The gabbro contains talc-carbonate veins."	"coarse grain gabbro with grain size variation cut by white veins."	
"399"	"U1601"	"C"	"151"	"R"	"2"	""	"399-U1601C-151R-2"	"0.0"	"141.0"	"747.145"	"747.850"	"748.555"	"747.145"	"747.85"	"748.555"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is a medium-grained granular olivine-bearing gabbro with variation in crystal size and texture on ~10 cm scale. It is a continuation from the overlying core."	"Variably altered Ol-gabbro. The extent of alteration increases toward hydrothermal veins. Plagioclase is altered to prehnite, chlorite, and secondary plagioclase close to the veins, while it is altered to chlorite far from the veins. Olivine is potentially replaced by clay and sulfide. The gabbro contains talc-prehnite-carbonate veins."	"isotropic gabbro with microfaulted interval cut by talc veins."	
"399"	"U1601"	"C"	"151"	"R"	"3"	""	"399-U1601C-151R-3"	"0.0"	"130.0"	"748.555"	"749.205"	"749.855"	"748.555"	"749.205"	"749.855"	""	"1, 2, 03, 04, 05, 06, 07, 08, 09, 10, 11, 12, 13"	""	"Most of this section is gabbro with variation in crystal size and texture on ~10 cm scale. It is a continuation from the overlying core. The gabbro unit contains serveral perodotite intervals."	"Variably altered Ol-gabbro and highly serpentinized harzburgite. The latter is cut by one hydrothermally altered magmatic vein made of chlorite, prehnite, secondary plagioclase, and reddish-brown Cpx. Opx in harzburgite decreases toward the contact with gabbro. The extent of alteration increases toward hydrothermal veins and the contact of serpentinite and gabbro. Spinel is fresh. Plagioclase is altered to prehnite, chlorite, and secondary plagioclase. Cpx is replaced by amphibole. Olivine is potentially replaced by clay and sulfide. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins. The gabbro contains talc-chlorite-carbonate veins and zeolite veins."	"gabbro, microfaulted, above dunite and protogranular serp harz, weak serp mesh foliation (0deg) cut by magmatic and talc veins."	
"399"	"U1601"	"C"	"151"	"R"	"4"	""	"399-U1601C-151R-4"	"0.0"	"58.0"	"749.860"	"750.150"	"750.440"	"749.86"	"750.15"	"750.44"	""	"1, 2, 3, 4"	""	"The section consists of harzburgite with 20% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite. The mesh is grey and black. Bastite is green, grey, and black. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a set of fibrous to massive chrysotile veins"	"protogranular serp harz, reg mesh with subvertical mantle fabric."	
"399"	"U1601"	"C"	"152"	"R"	"1"	""	"399-U1601C-152R-1"	"0.0"	"149.0"	"750.500"	"751.245"	"751.990"	"750.5"	"751.245"	"751.99"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"From 0-103 cm, harzburgite continues from the overlying section, but has15% orthopyroxene. Deformed course-grained gabbro makes up most of the rest of the section, although a small dunite domain is present at c. 130 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of plagioclase, chlorite, and secondary plagioclase. Brown stain within the vein. Slightly altered gabbro (99-121 cm) cut by chlorite vein. The mesh is grey and black. Bastite is grey and green. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"protogranular serp harz, reg mesh, above strongly foliated gabbro with isotropic contact, above talc schist with fault contact."	
"399"	"U1601"	"C"	"152"	"R"	"2"	""	"399-U1601C-152R-2"	"0.0"	"148.0"	"751.990"	"752.730"	"753.470"	"751.99"	"752.73"	"753.47"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Orthopyroxene-bearing dunite at the top grades to harzburgite with 10% orthopyroxene at c. 6 cm, down to 86 cm. A medium-grained equigranular gabbro with bimodal grain size cuts the section between 86 and 119 cm. A microgabbro pebble occurs at the interval of 107-113 cm. below 119 cm is an orthopyroxene-bearing dunite."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic veins made of chlorite and secondary plagioclase. Moderately altered gabbro (97-106 cm) cut by chlorite veins. Mesh is brown and black. Bastite is black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"serp harz, protomylonitic with strong foliated serp mesh. Not clear if protomylonitic deformation is mantle related or exhumation related, as serp mesh and mylonite foliation are not always parallel. Gabbro protomylonite interval."	
"399"	"U1601"	"C"	"152"	"R"	"3"	""	"399-U1601C-152R-3"	"0.0"	"123.0"	"753.470"	"754.085"	"754.700"	"753.47"	"754.085"	"754.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Most of the section is harzburgite with 10% orthopyroxene and trace chromium spinel. A medium-grained granular gabbro domain is disseminated in the host harzburgite at c. 48, 77, 87, and 92 cm."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, plagioclase, chlorite, prehnite, and secondary plagioclase. Brown stain within the vein, possibly on clinopyroxene. Mesh is brown and black. Bastite is green and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular to strong porphyroclastic (0deg) serp harz, weak foliated mesh (0deg). Small interval of harz has cp protomylonite fabric.  All cut by magmatic and white veins"	
"399"	"U1601"	"C"	"153"	"R"	"1"	""	"399-U1601C-153R-1"	"0.0"	"144.0"	"755.400"	"756.120"	"756.840"	"755.4"	"756.12"	"756.84"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"From the top to 64 cm is altered harzburgite with 13% orthopyroxene and trace spinel. Below 64 cm are olivine gabbros that coarsen in grain size down section (clinopyroxene grains are as large as 6 cm)."	"Highly serpentinized harzburgite/Opx-bearing dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, chlorite, and secondary plagioclase. Brown stain within the vein, possibly on clinopyroxene. Slightly to moderately altered gabbro (64-144 cm) cut by zeolite veins and one talc vein. Mesh is brown and grey. Bastite is green and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular to strong porphyroclastic (20deg) serp harz, reg to weak foliated mesh (15deg). Gabbro interval, grain variation, rarely fractured"	
"399"	"U1601"	"C"	"153"	"R"	"2"	""	"399-U1601C-153R-2"	"0.0"	"150.0"	"756.840"	"757.590"	"758.340"	"756.84"	"757.59"	"758.34"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The entire section is olivine gabbro with varying gran sizes, coarse grained at the top, and medium grained in the middle."	"Moderately altered Ol-bearing gabbro to pegmatitic gabbro cut by prehnite-chlorite veins, zeolite, and amphibole veins. The extent of alteration increases down section. In places, sulfides occur in association with relict olivine."	"isotropic to magmatically foliated (45deg) GABBRO, WITH GRAIN SIZE LAYERING AND MODAL LAYERING."	
"399"	"U1601"	"C"	"153"	"R"	"3"	""	"399-U1601C-153R-3"	"0.0"	"144.0"	"758.340"	"759.060"	"759.780"	"758.34"	"759.06"	"759.78"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Course grained olivine gabbro down to 83 cm, with orthopyroxene-bearing dunite below grading to harzburgite with average 12% orthopyroxene beneath 117 cm. Trace chromium spinel is present in the peridotites, and most of the orthopyroxene is interstitial."	"Highly altered gabbro cut by talc-carbonate and zeolite veins. Highly serpentinized Opx-bearing dunite to harzburgite. Mesh is brown to black. Bastite is green to black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and one massive picrolite vein."	"gabbro with strongly foliated (deformaion) intervals with a brittle fracture overprint, above serp harz, protogranular serp harz with weak mesh (30deg) and several piece end faults"	
"399"	"U1601"	"C"	"154"	"R"	"1"	""	"399-U1601C-154R-1"	"0.0"	"140.5"	"760.200"	"760.903"	"761.605"	"760.2"	"760.903"	"761.605"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly orthopyroxene-bearing dunite (ave. 8 % orthopyroxene) grading to harzburgite (ave. 12% orthopyroxene) below 114 cm. Two small (2-10 mm) pervasively altered gabbroic veins are present above 78 cm."	"Highly serpentinized Opx-bearing dunite to harzburgite; the former is cut by a hydrothermally altered magmatic vein made of plagioclase, clinopyroxene, secondary plagioclase, and chlorite. Mesh is brown to black. In Opx-bearing dunite bastite is black. Bastite is green in harzburgite. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins"	"protogranular serp harz, reg to weak foliated mesh (0deg)"	
"399"	"U1601"	"C"	"154"	"R"	"2"	""	"399-U1601C-154R-2"	"0.0"	"139.0"	"761.605"	"762.300"	"762.995"	"761.605"	"762.3"	"762.995"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is harzburgite with 12 % orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite and harzburgite. Mesh is brown to black. In dunite bastite tends to be black and greenish in harzburgite. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a network of fibrous to massive chrysotile veins."	"protogranular serp harz, reg mesh"	
"399"	"U1601"	"C"	"154"	"R"	"3"	""	"399-U1601C-154R-3"	"0.0"	"131.0"	"762.995"	"763.650"	"764.305"	"762.995"	"763.65"	"764.305"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"The harzburgite from the overlying section continues down to 26 cm. A coarse-grained, granular olivine-bearing gabbro makes up the rest of the section. It has significant grain size variations on a centimeter to decimeter scale. "	"Variably altered gabbro and highly serpentinized Opx-bearing dunite cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, and secondary plagioclase. Prehnite is abundant at the contact with dunite. The gabbro is cut by chlorite, zeolite, and prehnite-carbonate veins. Mesh is brown to black. Bastite is black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg mesh. gabbro interval, fractured in places, lots of white veins"	
"399"	"U1601"	"C"	"155"	"R"	"1"	""	"399-U1601C-155R-1"	"0.0"	"132.0"	"765.100"	"765.760"	"766.420"	"765.1"	"765.692"	"766.283"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Most of this section is orthopyroxene-bearing dunite with trace chromium spinel. A harzburgite with an average of 12 % orthopyroxene and trace spinel and clinopyroxene is between 63 and 95 cm. A coarse-grained granular gabbro makes up the topmost 6.5 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite cut by one hydrothermally altered magmatic vein made of clinopyroxene, chlorite, and secondary plagioclase. One piece of moderately altered gabbro at the top of the section. Clinopyroxene is fresh in gabbro. Gabbro is cut by chlorite and zeolite veins. Mesh is black to grey. Bastite is green in harzburgite, while black bastite is dominant in dunite. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular serp harz, reg to weakly foliated (0-30deg) mesh. small gabbo interva;l"	
"399"	"U1601"	"C"	"155"	"R"	"2"	""	"399-U1601C-155R-2"	"0.0"	"150.0"	"766.420"	"767.170"	"767.920"	"766.283"	"766.956"	"767.628"	""	"1, 2, 3, 4, 5"	""	"This section is entirely orthopyroxene-bearing dunite averaging about 8% orthopyroxene, with trace spinel and clinopyroxene (?)."	"Highly serpentinized Opx-bearing dunite and harzburgite; both are cut by hydrothermally altered magmatic veins made of clinopyroxene (brown stain) and secondary plagioclase. The mesh is black to grey. Bastite is black and locally green. Some relicts of fresh orthopyroxene and olivine (variable extent of serpentinization). Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"protogranular to porphyroclastic (10deg) serp harz, no mesh to weakly foliated mesh (10deg)"	
"399"	"U1601"	"C"	"155"	"R"	"3"	""	"399-U1601C-155R-3"	"0.0"	"133.0"	"767.920"	"768.585"	"769.250"	"767.628"	"768.224"	"768.82"	""	"1, 2, 3"	""	"Orthopyroxene-bearing dunite grading down to dunite at 101 cm. Trace chromium spinel is throughout. Two cm-sized websterite clots are at c. 82 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite. The mesh is black, grey, and brown. Bastite is green and locally black. The contact between harzburgite and dunite contains two large grains of pyroxene which are fresh. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins."	"protogranular to porphyroclastic (0deg) serp harz and dunit, weakly foliated mesh (0deg)"	
"399"	"U1601"	"C"	"155"	"R"	"4"	""	"399-U1601C-155R-4"	"0.0"	"120.5"	"769.250"	"769.852"	"770.455"	"768.82"	"769.362"	"769.904"	""	"1, 2, 3"	""	"Dunite grading down to orthopyroxene-bearing dunite at 23 cm. Trace chromium spinel is throughout."	"Highly serpentinized Opx-bearing dunite and harzburgite; the former is cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, secondary plagioclase, and chlorite. Mesh is brown to grey. Bastite is black in dunite and green in harzburgite. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, and fibrous to massive chrysotile veins. The latter cut through the magmatic vein."	"protogranular to porphyroclastic (15deg) serp harz and dunite, weakly to strongly foliated mesh (0-15deg)"	
"399"	"U1601"	"C"	"156"	"R"	"1"	""	"399-U1601C-156R-1"	"0.0"	"92.0"	"769.900"	"770.360"	"770.820"	"769.9"	"770.36"	"770.82"	""	"1, 2, 3"	""	"This section is harzburgite with 15 % orthopyroxene (mostly granular) and trace clinopyroxene and chromium spinel. The orthopyroxene percentage decreases down section."	"Highly serpentinized harzburgite. Mesh is black and brown and locally greenish. Bastite is green and locally brown; light brown bastite is possibly after Cpx. Bastite is black close to a chlorite-amphibole vein. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and massive serpentine, chlorite, and chlorite-amphibole veins."	"protogranular serp harz with regular to weak foliated (10deg) mesh"	
"399"	"U1601"	"C"	"156"	"R"	"2"	""	"399-U1601C-156R-2"	"0.0"	"146.0"	"770.820"	"771.550"	"772.280"	"770.82"	"771.55"	"772.28"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite down to 83 cm with an average of 17% orthopyroxene and multiple trails of chromium spinel. Below 90 cm is dunite with variable proportions of orthopyroxene and chromium spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of chlorite, prehnite, and amphibole. Highly fractured serpentinite slickenside is present. The extent of serpentinization is variable. More abundant relict olivine exists close to bastite. Chrysotile vein density is high. The mesh is black. Bastite is green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and massive picrolite."	"protogranular serp harz and dunite with regular to weak foliated (10deg) mesh"	
"399"	"U1601"	"C"	"156"	"R"	"3"	""	"399-U1601C-156R-3"	"0.0"	"118.0"	"772.280"	"772.870"	"773.460"	"772.28"	"772.87"	"773.46"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"The section down to 54 cm is intermixed harzburgite (15% orthopyroxene) and highly altered gabbros (42-45 cm, 51-54 cm). Below 54 cm is orthopyroxene bearing dunite with highly altered gabbro horizons at 69-72, 79-92, and 95 cm. Trace chromium spinel is found throughout the peridotites."	"Highly serpentinized Opx-bearing dunite to harzburgite cut by hydrothermally altered magmatic veins made of plagioclase, clinopyroxene, chlorite, and secondary plagioclase. Moderately altered gabbro (76-91 cm) cut by amphibole, talc-carbonate, and white (possibly quartz) veins. At the contact between gabbro and serpentinite, both rocks are highly deformed. The mesh is grey to brown. Bastite is black, grey, and green. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chysotile veins, and massive picrolite veins. The latter cut through the magmatic veins."	"protogranular serp harz with faulted cotnact against protomylonitic gabbro. white veins cut gabbro mylonite but not harz, some veins are possibly sheared, whereas other ar not - not clear if veins pre- or post-date mylonite"	
"399"	"U1601"	"C"	"156"	"R"	"4"	""	"399-U1601C-156R-4"	"0.0"	"122.0"	"773.460"	"774.070"	"774.680"	"773.46"	"774.07"	"774.68"	""	"1, 2, 3, 4"	""	"The section is intermixed harzburgite (11% orthopyroxene, trace chromium spinel) and highly altered gabbros (35-37 cm, 48-49 cm). "	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic veins made of clinopyroxene, amphibole, plagioclase, chlorite, and secondary plagioclase. Mesh is brown to black. Bastite is black and locally green. Spinel has red-brown stain. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, fibrous to massive chrysotile veins, and massive picrolite. The latter cut through the magmatic veins"	"protogranular serp harz with regular patchy mesh"	
"399"	"U1601"	"C"	"157"	"R"	"1"	""	"399-U1601C-157R-1"	"0.0"	"79.0"	"774.800"	"775.195"	"775.590"	"774.8"	"775.195"	"775.59"	""	"1, 2, 3, 4, 5, 6"	""	"This section is predominantly harzburgite with about 13 percent orthopyroxene, mostly granular, and trace chromium spinel. A pebble of highly altered, medium-grained melagabbro makes up the section below 64.5 cm."	"Highly serpentinized harzburgite and a small piece of altered gabbro at the bottom of the section. Mesh is grey, brown, and black. Bastite is black and green. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and fibrous to massive chrysotile veins."	"protogranular serp harz, reg mesh"	
"399"	"U1601"	"C"	"157"	"R"	"2"	""	"399-U1601C-157R-2"	"0.0"	"139.0"	"775.590"	"776.285"	"776.980"	"775.59"	"776.285"	"776.98"	""	"1, 2, 3, 4"	""	"This section is predominantly harzburgite with 15 down to 10 % orthopyroxene, mostly granular, and trace chromium spinel. Gabbro veins cut the harzburgite at 63 and and 114-121 cm."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein made of clinopyroxene, amphibole, plagioclase, and secondary plagioclase. Small piece of altered gabbro (114-121 cm). Some mesh areas appear greyish with black bastite while other areas are more blackish with green bastite, but the extent of serpentinization remains similar (difference in magnetite content?). Mesh is grey, brown, and black. Bastite is mainly green and locally black. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and fibrous to massive chrysotile veins."	"protogranular serp harz, reg mesh. 122-139cm sheared magnetite-serpentine veins cut across background fabric with protomylonitic CP deformation."	
"399"	"U1601"	"C"	"157"	"R"	"3"	""	"399-U1601C-157R-3"	"0.0"	"141.0"	"776.980"	"777.685"	"778.390"	"776.98"	"777.685"	"778.39"	""	"1, 2, 3, 4, 5, 6"	""	"This section is predominantly harzburgite with 17 % orthopyroxene, mostly granular, and trace chromium spinel. "	"Highly to completely serpentinized harzburgite. Mesh is green to black. Bastite is mainly green. Locally talc after orthopyroxene. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"protogranular to porphyroclastic (85-90deg) serp harz, no mesh to weak fol (10deg) mesh."	
"399"	"U1601"	"C"	"157"	"R"	"4"	""	"399-U1601C-157R-4"	"0.0"	"113.0"	"778.390"	"778.955"	"779.520"	"778.39"	"778.955"	"779.52"	""	"1, 2, 3, 4, 5, 6"	""	"This section is mostly harzburgite with 10-12 % orthopyroxene,  and trace chromium spinel. A highly altered gabbro domain is present in the lower few cm of the section"	"Highly serpentinized harzburgite and altered gabbro at the bottom of the section (105-113 cm). The mesh is black to grey. Bastite is green and black. Locally talc forms after orthopyroxene. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"protogranular serp harz, no mesh"	
"399"	"U1601"	"C"	"158"	"R"	"1"	""	"399-U1601C-158R-1"	"0.0"	"143.0"	"779.600"	"780.315"	"781.030"	"779.6"	"780.315"	"781.03"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Most of this section is harzburgite with minimal orthopyroxene and trace chromium spinel. Highly altered gabbro domains are found at 0-4 and between 43 and 97 cm. Aphyric diabase composes the core from 43 to 79 cm. "	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins (rubble) made of plagioclase, clinopyroxene, chlorite, prehnite, amphibole, an unidentified orange-brown mineral (zeolite or plagioclase/clays mixture?), and secondary plagioclase. Mesh is brown to black. Bastite is green and black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"protogranular serp harz, weak mesh, rubble with gabbro mylonite and diabase."	
"399"	"U1601"	"C"	"158"	"R"	"2"	""	"399-U1601C-158R-2"	"0.0"	"132.0"	"781.030"	"781.690"	"782.350"	"781.03"	"781.69"	"782.35"	""	"1, 2, 3"	""	"This section is mostly harzburgite with 12-13 % orthopyroxene (granular and interstitial) and trace chromium spinel. The interval between 48 and 65 cm is orthopyroxene-bearing dunite."	"Highly serpentinized harzburgite and dunite; the latter is cut by one hydrothermally altered magmatic vein made of plagioclase, clinopyroxene, and amphibole. Brown stain within the vein. The mesh is grey to black. Bastite is green and black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins whose abundance decreases in dunite, and massive picrolite veins. The latter cut through the magmatic vein."	"protogranular to porphyroclastic (10deg) serp harz, no mesh to reg mesh."	
"399"	"U1601"	"C"	"158"	"R"	"3"	""	"399-U1601C-158R-3"	"0.0"	"120.0"	"782.350"	"782.950"	"783.550"	"782.35"	"782.95"	"783.55"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Orthopyroxene-bearing dunite to harzburgite with trace chromium spinel. A thin highly altered gabbroic vein cuts the section at 30 cm. "	"Highly to completely serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic veins made of amphibole, chlorite, prehnite, and secondary plagioclase. Mesh is brown to black. Bastite is green to brown to black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"protogranular to porphyroclastic (10deg) serp harz, reg mesh."	
"399"	"U1601"	"C"	"159"	"R"	"1"	""	"399-U1601C-159R-1"	"0.0"	"150.0"	"784.500"	"785.250"	"786.000"	"784.5"	"785.25"	"786"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Most of the section is harzburgite with 12 % orthopyroxene and trace chromium spinel. The base of the section below 109 cm is altered, coarse grained and granular gabbro."	"Highly serpentinized harzburgite to Opx-bearing dunite; the latter is cut by one hydrothermally altered magmatic vein made of plagioclase, amphibole, and chlorite. Brown stain within the vein. Highly altered gabbro (107-135 cm) cut by chlorite veins. Mesh is black to grey to brown. Bastite is black and green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic vein."	"protogranular to porphyroclastic (15deg) serp harz, reg mesh."	
"399"	"U1601"	"C"	"159"	"R"	"2"	""	"399-U1601C-159R-2"	"0.0"	"121.5"	"786.000"	"786.607"	"787.215"	"786"	"786.607"	"787.215"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 14% orthopyroxene and trace chromium spinel down to 25 cm. It is underlain by dunite with varying proportions of orthopyroxene and chromium spinel."	"Highly to completely serpentinized Opx-bearing dunite/harzburgite. Mesh is brown to black. Bastite is green to black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chysotile veins, and massive picrolite veins."	"protogranular to porphyroclastic (0-15deg) serp harz, reg to weakly foliated (0-15deg) mesh. Multiple piece-end faults"	
"399"	"U1601"	"C"	"159"	"R"	"3"	""	"399-U1601C-159R-3"	"0.0"	"105.0"	"787.215"	"787.740"	"788.265"	"787.215"	"787.74"	"788.265"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The upper 60 cm of this section is oxide gabbro, much of which is mylonitized. The base of the section is dunite with more than 1% chromium spinel."	"Moderately altered gabbro and highly serpentinized Opx-bearing dunite cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. The gabbro is cut by amphibole veins. The mesh is black to brown. Bastite is black. Spinel is fresh and is abundant near the contact with gabbro. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a set of fibrous to massive chrysotile veins"	"gabbro mylonite, above dunite , normal fault"	
"399"	"U1601"	"C"	"160"	"R"	"1"	""	"399-U1601C-160R-1"	"0.0"	"135.0"	"789.300"	"789.975"	"790.650"	"789.3"	"789.975"	"790.65"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"The top 5 cm contains a harzburgite pebble that may be accidental. Most of the rest of the core is dunite with 1% chromium spinel and trace orthopyroxene. Gabbro veins cut the section at 49 and 63 cm."	"Highly serpentinized Opx-bearing, and possibly Cpx-bearing, dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. Mesh is black to brown. Bastite is black and white; the latter possibly after clinopyroxene. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through the magmatic veins."	"dunite, very dark black, weak fol mesh (0deg), cut by several magmatic veins (50-70deg)."	
"399"	"U1601"	"C"	"160"	"R"	"2"	""	"399-U1601C-160R-2"	"0.0"	"146.0"	"790.650"	"791.380"	"792.110"	"790.65"	"791.38"	"792.11"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section consists of orthopyroxene-bearing dunite with abundant chromium spinel. One spinel grain is 2 cm in length. The orthopyroxenes are mainly interstitial with abundance varying from trace to 8 wt%. "	"Highly serpentinized pyroxene-bearing dunite/wherlite. Mesh is brown to black. Bastite is green, light brown, or black. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and massive picrolite veins."	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"160"	"R"	"3"	""	"399-U1601C-160R-3"	"0.0"	"149.0"	"792.110"	"792.855"	"793.600"	"792.11"	"792.855"	"793.6"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section consists of orthopyroxene-bearing dunite to dunite with trace chromium spinel."	"Highly serpentinized Px-bearing dunite/wherlite. Mesh is brown to black. Bastite is black to light brown (the latter possibly after clinopyroxene). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a network of fibrous to massive chrysotile veins, and three massive unidentified green-black veins."	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"161"	"R"	"1"	""	"399-U1601C-161R-1"	"0.0"	"141.0"	"794.200"	"794.905"	"795.610"	"794.2"	"794.905"	"795.61"	""	"1, 2"	""	"Most of this section is dunite with trace chromium spinel."	"Highly serpentinized dunite and pyroxene-bearing dunite (top of the section, 0-11 cm) cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. Mesh is brown to black to greenish grey. Bastite is light brown (possibly after clinopyroxene) to green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chysotile veins, and massive picrolite veins. The latter cut through magmatic veins"	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"161"	"R"	"2"	""	"399-U1601C-161R-2"	"0.0"	"133.0"	"795.610"	"796.275"	"796.940"	"795.61"	"796.275"	"796.94"	""	"1, 2, 3, 4"	""	"Dunite with abundant chromium spinel (2%)."	"Highly to completely serpentinized and deformed peridotite (original mineralogy is not known) cut by one hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, secondary plagioclase, chlorite, amphibole, and prehnite. The identification of mesh is hard. Bastite is light brown (possibly after clinopyroxene) at the bottom of the section (127-130 cm). Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a set of fibrous to massive chrysotile veins."	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"161"	"R"	"3"	""	"399-U1601C-161R-3"	"0.0"	"139.0"	"796.940"	"797.635"	"798.330"	"796.94"	"797.635"	"798.33"	""	"1"	""	"Dunite with abundant chromium spinel (1%) at the top. The lithology grades downward to orthopyroxene-bearing dunite with only trace chromium spinel. "	"Highly to completely serpentinized Px-bearing dunite/wherlite. The mesh is black to brown. Bastite is light brown (possibly after clinopyroxene) to black. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and one massive black vein rimmed by chrysotile veins."	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"161"	"R"	"4"	""	"399-U1601C-161R-4"	"0.0"	"67.0"	"798.330"	"798.665"	"799.000"	"798.33"	"798.665"	"799"	""	"1, 2"	""	"This section is orthopyroxene-bearing dunite with trace chromium spinel and mainly interstitial orthopyroxene. The abundance of orthopyroxene varies from 0.1 to 9 %."	"Highly to completely serpentinized Px-bearing dunite/wherlite. Mesh is black to brown to grey. Bastite is light brown (possibly after clinopyroxene) to black. Spinel is fresh. The serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture and a set of fibrous to massive chrysotile veins."	"opx-dunite with subvertical protomylonitic sections deforming opx grains, but overprinted by undeformed cpx grains"	
"399"	"U1601"	"C"	"162"	"R"	"1"	""	"399-U1601C-162R-1"	"0.0"	"145.0"	"799.000"	"799.725"	"800.450"	"799"	"799.622"	"800.245"	""	"1, 2, 3, 4, 5"	""	"Peridotite with varying proportions (trace to 10%) of largely interstitial orthopyroxene and trace to 1%, relatively coarse-grained spinel."	"Highly to completely serpentinized dunite to Px-bearing dunite/wherlite. Mesh is black to brown to grey. Bastite is light brown (possibly after clinopyroxene) to black. Mesh-forming veins and chrysotile veins."	"serpentinized harzburgite and dunite, vertical SPO, horizontal mesh"	
"399"	"U1601"	"C"	"162"	"R"	"2"	""	"399-U1601C-162R-2"	"0.0"	"142.0"	"800.490"	"801.200"	"801.910"	"800.279"	"800.888"	"801.497"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Dunite and orthopyroxene-bearing dunite with varying proportions (trace to 6%) of largely interstitial orthopyroxene and trace to 0.5%, relatively coarse-grained spinel. A highly altered gabbro domain 30-35mm in width and the host dunite at 93-105 cm and 132-140 cm."	"Highly to completely serpentinized dunite to Px-bearing dunite/wherlite cut by hydrothermally altered magmatic vein made of Cpx, plagioclase, amphibole, chlorite, and possibly secondary plagioclase. The mesh is black, green to grey. Sulfide is locally associated with mesh. Bastite is light brown (possibly after clinopyroxene) to black, and green. Mesh-forming serpentine + magnetite, chrysotile, picrolite, and magmatic veins."	"serpentinized harzburgite and dunite, vertical SPO, horizontal mesh, big steep magmatic veins"	
"399"	"U1601"	"C"	"162"	"R"	"3"	""	"399-U1601C-162R-3"	"0.0"	"134.0"	"801.940"	"802.610"	"803.280"	"801.523"	"802.098"	"802.673"	""	"1, 2, 3, 4, 5"	""	"Dunite with trace, largely granular orthopyroxene."	"Highly serpentinized dunite cut by a magmatic vein of plagioclase and Cpx. Mesh is black to grey and locally brown. Sulfide occurs in brown mesh. Mesh-forming serpentine + magnetite, chrysotile, picrolite, and magmatic veins."	"dunite with a weakly foliated serpentine fabric (10deg) cross cut by a magmatic vein (70deg) and several slicked white veins with shallow to moderate plunges."	
"399"	"U1601"	"C"	"162"	"R"	"4"	""	"399-U1601C-162R-4"	"0.0"	"143.0"	"803.280"	"803.995"	"804.710"	"802.673"	"803.287"	"803.9"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Orthopyroxene-bearing dunite with 1-6 %, largely granular orthopyroxene."	"Highly serpentinized Opx-bearing dunite. The mesh is black to grey. Bastite is green. Mesh-forming serpentine + magnetite, and chrysotile veins."	"Weakly to strongly foliated serpentine foliation in dunite (10deg) with shallow little white veins and several white and/or green slicked veins (35-80deg) with moderate to steep plunges, two with reverse sense of shear."	
"399"	"U1601"	"C"	"162"	"R"	"CC"	""	"399-U1601C-162R-CC"	"0.0"	"18.0"	"804.410"	"804.500"	"804.590"	"803.742"	"803.821"	"803.9"	""	""	""	"Orthopyroxene-bearing dunite with c. 7% granular orthopyroxene."	"Highly serpentinized Opx-bearing dunite. The mesh is black to grey. Bastite is green. Mesh-forming serpentine + magnetite, and chrysotile veins."	"Weakly to strongly foliated serpentine foliation in dunite (10deg) with shallow little white veins and several white and/or green slicked veins (35-80deg) with moderate to steep plunges, two with reverse sense of shear."	
"399"	"U1601"	"C"	"163"	"R"	"1"	""	"399-U1601C-163R-1"	"0.0"	"146.0"	"803.900"	"804.630"	"805.360"	"803.9"	"804.63"	"805.36"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Dunite with 1% chromium spinel down to 9 cm. The dunite is underlain by a fault zone down to 70 cm. The upper parts of this fault zone consist of diorite with 40% amphibole, and 15% fragments of diabase and dunite. Between 28 and 70 cm are fragmented domains of diabase and gabbro along with fragments of gabbro and ultramafic lithologes. Below 70 cm, the section consists of two domains: harzburgite with minimal orthopyroxene and trace chromium spinel, and highly altered gabbro."	"Highly altered gabbro and highly serpentinized Px-bearing dunite. Gabbro contains sulfides in brown areas, possibly after olivine. Alternatively, it could be slivers of dunite completely metasomatized. The gabbro is cut by carbonate-talc-prehnite-sulfide and carbonate veins. Mesh is black to grey to brown. Bastite is light brown (possibly after clinopyroxene) to black to green. Spinel is fresh. Serpentinite contains several types of veins, including serpentine-magnetite veins in mesh texture, a set of fibrous to massive chrysotile veins, and carbonate veins connect to those cutting through the gabbro."	"dunite, undeformed to ultramylonitic gabbro, harzburgite cut by dark vein and harzburgite which is partially protomylonitic , mostly rubble"	
"399"	"U1601"	"C"	"163"	"R"	"2"	""	"399-U1601C-163R-2"	"0.0"	"133.0"	"805.360"	"806.025"	"806.690"	"805.36"	"806.025"	"806.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"The harzburgite from the overlying section continues through the top 8 cm in this section together with gabbroic veins. The remainder of the section is medium grained, granular sulfide-bearing oxide gabbro "	"Slightly altered olivine-bearing gabbro and piece of highly serpentinized Opx-bearing dunite at the top of the section. Bastite is grey, black, and green. Mesh is brown to black. Several serpentine vein generations as well as carbonate-sulfide veins in serpentinite. Gabbro contains chlorite veins and carbonate veins."	"oxide gabbro, protomytlonite - lots of small unoriented peices, variable strain, some less deformed intervals."	
"399"	"U1601"	"C"	"163"	"R"	"3"	""	"399-U1601C-163R-3"	"0.0"	"85.0"	"806.820"	"807.245"	"807.670"	"806.82"	"807.245"	"807.67"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is oxide gabbro and oxide-bearing gabbro continued from the overlying section."	"Slightly altered coarse grained gabbro. Locally plagioclase and Cpx have brown stain. The gabbro features a network of zeolite veinlets and one talc-carbonate vein."	"Ox-gabbro, isotropic cut by shallow to moderately dipping veins."	
"399"	"U1601"	"C"	"164"	"R"	"1"	""	"399-U1601C-164R-1"	"0.0"	"146.0"	"808.700"	"809.430"	"810.160"	"808.7"	"809.43"	"810.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This section consists of oxide and oxide-bearing gabbro with trace sulfides."	"Slightly altered coarse grained oxide-gabbro containing chalcopyrite and pyrrhotite.  Locally Cpx has a brown stain. Zeolite, chlorite, amphibole, and talc-carbonate veins can be observed."	"dark grey gabbro wih talc veins unoriented, caorse grained isotropic. ox-gabbro has matrix of oxide surrounding cpx"	
"399"	"U1601"	"C"	"164"	"R"	"2"	""	"399-U1601C-164R-2"	"0.0"	"146.0"	"810.160"	"810.890"	"811.620"	"810.16"	"810.89"	"811.62"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section consists of coarse-grained granular gabbro with plagioclase proportions decreasing down section. At the end is a pile of pebbles with one pebble of orthopyroxene-bearing dunite."	"Moderately altered gabbro with variable grain size. Cpx and plagioclase are locally brown-stained. Zeolite and talc-carbonate veins are present."	"ox-gabbro, isotropic, fractured with white veins filling fracturing"	
"399"	"U1601"	"C"	"164"	"R"	"3"	""	"399-U1601C-164R-3"	"0.0"	"107.0"	"811.620"	"812.155"	"812.690"	"811.62"	"812.155"	"812.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is mostly orthopyroxene-bearing dunite with trace chromium spinel. A coarse-grained gabbro cuts the section at 56-77 cm. It contains a poorly-preserved reaction boundary with overlying peridotites."	"Highly serpentinized Opx-bearing dunite with altered magmatic vein and moderately altered Ol-bearing gabbro. The hydrothermally altered magmatic vein contains brown stained Cpx and Plag. Gabbro has greenish-brown patch. Bastite color is grey and black. The mesh color is black and brown. Spinel is fresh. Several vein types composed of serpentine, sulfide-carbonate, talc-carbonate, and an altered magmatic vein are present in this section."	"porphyroclastic (65deg) serp harz, no mesh, above isotropic gabbro fractured."	
"399"	"U1601"	"C"	"165"	"R"	"1"	""	"399-U1601C-165R-1"	"0.0"	"120.5"	"813.600"	"814.202"	"814.805"	"813.6"	"814.202"	"814.805"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is mostly medium grained and granular gabbro. mylonitized in it slower portion. Orthopyroxene bearing dunite makes up the core from 0 to 6 cm. Harzburgite with 10 % orthopyroxene and trace chromium spinel is between 11.5 and 29 cm."	"Variably altered deformed Ol-bearing gabbro and highly serpentinized harzburgite containing hydrothermally altered magmatic vein composed of Cpx, plagioclase, amphibole, secondary plagioclase, sulfide, and chlorite. Patchy brown stain of Plag and Cpx near serpentinite contact. Several vein generations are present, including mesh, chrysotile, hydrothermally altered magmatic vein, amphibole, talc-carbonate, and amphibole-sulfide veins."	"complete gabbro interval with reverse sense strain gradient from mylonite at base to protomylonite at top, talc alteration overprints deformation fabric at top of gabbro interval. harz above and below is also protomylonite. gabbro mylonite fabric is cross cut by talc-carbonate veins."	
"399"	"U1601"	"C"	"165"	"R"	"2"	""	"399-U1601C-165R-2"	"0.0"	"150.0"	"814.805"	"815.555"	"816.305"	"814.805"	"815.555"	"816.305"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly orthopyroxene bearing dunite with trace chromium spinel. Medium grained, equigranular gabbro cuts the section from 29 to 55 cm. A coarse-grained gabbro is in contact with the peridotite from 85 to 113 cm."	"Highly serpentinized Opx-bearing dunite and highly altered gabbro. The dunite contains a hydrothermally altered magmatic vein. A pink mineral in gabbro may be zoisite. Bastite ranges from grey to black and within halo it is blue-green. The mesh is black to brown. Serpentine and serpentine-magnetite veins in serpentinite. Chlorite, zeolite, and hydrothermally altered magmatic veins in gabbro."	"Isotropic to mylonitic gabbro (30-45deg) with sheared serp harz that is protogranular; contacts are 40-45deg in dip. "	
"399"	"U1601"	"C"	"165"	"R"	"3"	""	"399-U1601C-165R-3"	"0.0"	"87.5"	"816.305"	"816.742"	"817.180"	"816.305"	"816.742"	"817.18"	""	"1, 2, 3"	""	"This section consists of harzburgite with 12% orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx bearing dunite with hydrothermally altered magmatic vein composed of Cpx and plagioclase. Cpx shows a brown stain. Spinel is fresh. Serpentine-magnetite, chrysotile, and one hydrothermally altered magmatic vein cut the serpentinite."	"porphyroclastic (25deg) serp harz, reg mesh"	
"399"	"U1601"	"C"	"166"	"R"	"1"	""	"399-U1601C-166R-1"	"0.0"	"139.0"	"818.400"	"819.095"	"819.790"	"818.4"	"819.095"	"819.79"	""	"1, 2, 3, 4, 5, 6"	""	"Most of this section is harzburgite with 15 % orthopyroxene, including some rounded granular grains. A medium-grained granular gabbroic vein 5mm wide crosscuts the host harzburgite."	"Highly serpentinized harzburgite and Opx-bearing dunite/harzburgite. The latter is cut by one hydrothermally altered magmatic vein, composed of Cpx (with brown stain), plagioclase, secondary plagioclase, and prehnite. Fresh spinel. Bastite is green in harzburgite and black to grey in dunite. Mesh is black to brown in dunite and grey-ish in harzburgite. Serpentine, serpentine-magnetite, and one hydrothermally altered magmatic vein."	"porphyroclastic (10-55deg) serp harz, reg mesh to no mesh"	
"399"	"U1601"	"C"	"166"	"R"	"2"	""	"399-U1601C-166R-2"	"0.0"	"150.0"	"819.790"	"820.540"	"821.290"	"819.79"	"820.54"	"821.29"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is mostly peridotites, mainly harzburgite and a central section of orthopyroxene-bearing dunite. The dunite borders a coarse-grained gabbroic domain."	"Highly serpentinized harzburgite and gabbro. Bastite is green to grey. The mesh is black and brown to grey. Various flavors of serpentine-bearing veins. Zeolite and prehnite-carbonate-chlorite veins in gabbro."	"protogranular serp harz, reg to weak fol (0deg) mesh, gabbro interval, isotropic undeformed"	
"399"	"U1601"	"C"	"167"	"R"	"1"	""	"399-U1601C-167R-1"	"0.0"	"131.0"	"823.300"	"823.955"	"824.610"	"823.3"	"823.909"	"824.519"	""	"1, 2"	""	"This section is harzburgite with 12 % orthopyroxene, including some rounded granular grains, as well as trace chromium spinel. "	"Highly serpentinized Opx-bearing dunite and harzburgite. Opx content is variable. Cut by magmatic vein composed of Cpx, plagioclase secondary plagioclase, and chlorite. Brown stain. Bastite is green and black. Mesh is black to brown and grey (mottled). Spinel is fresh. The serpentinite is cut by several serpentine-bearing vein types including mesh, chrysotile, and picrolite veins, as well as several hydrothermally altered magmatic veins."	"protogranular serp harz, reg to weak fol (10deg) mesh"	
"399"	"U1601"	"C"	"167"	"R"	"2"	""	"399-U1601C-167R-2"	"0.0"	"127.0"	"824.610"	"825.245"	"825.880"	"824.519"	"825.11"	"825.7"	""	"1, 2, 3, 4, 05, 06, 7, 8"	""	"This section is harzburgite with 12 % orthopyroxene, including some rounded granular grains, as well as trace chromium spinel. It grades downward to orthopyroxene-bearing dunite in the middle of the section. "	"Highly serpentinized Opx-bearing dunite and harzburgite cut by magmatic vein composed of clinopyroxene, plagioclase, second plagioclase, and chlorite. Bastite is greyish and black, locally green. Small amount of light brown bastite, possibly after clinopyroxene. Mesh is black to brown and grey (mottled). Spinel is fresh. The serpentinite is cut by several serpentine-bearing vein types including mesh, chrysotile, and picrolite veins. The latter cut through the magmatic vein."	"weakly porphyroclastic serp harz to protogranular harz with regular mesh"	
"399"	"U1601"	"C"	"167"	"R"	"3"	""	"399-U1601C-167R-3"	"0.0"	"147.0"	"825.880"	"826.615"	"827.350"	"825.7"	"826.384"	"827.067"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly gabbro. The upper 56 cm is a pegmatitic, granular gabbro; from 56 to 78 cm, it is a medium-grained oxide-bearing gabbro. From 78 to 115 cm is a medium-grained granular gabbro. the basal 8 cm is orthopyroxene-bearing dunite with trace chromium spinel."	"Variably altered coarse-grained to pegmatitic Ol-bearing gabbro and highly serpentinized Opx-bearing dunite. Bastite is green. The mesh is black and green. Sulfides are disseminated in the gabbro associated with Plag and Ol. The extent of alteration increases toward the lower contact with serpentinite. Serpentine and serpentine-magnetite veins occur in serpentinite. Gabbro contains talc-carbonate-prehnite and zeolite veins."	"pegmatitic gabbro with protomylonitic intervals"	
"399"	"U1601"	"C"	"167"	"R"	"4"	""	"399-U1601C-167R-4"	"0.0"	"111.0"	"827.350"	"827.905"	"828.460"	"827.067"	"827.583"	"828.1"	""	"1, 2, 3, 4"	""	"This section is dunite with proportions of orthopyroxene varying from 0 to 9 %, and with trace to 1 % chromium spinel. The lowermost bin has a medium-grained gabbro pebble."	"Highly serpentinized harzburgite and dunite cut by altered. Magmatic vein containing Cpx (brown stained), plagioclase, and secondary plagioclase. Bastite varies from black to green and locally brown and light brown. Mesh varies from black, grey to brown. Brownish bastite occurs near the magmatic vein. Spinel is fresh. Serpentinite contains serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins."	"protogranular serp harz with regular mesh, dunite with regular mesh, contact between them is followed by a vein, lower part protogranular harzburgite with regular mesh"	
"399"	"U1601"	"C"	"168"	"R"	"1"	""	"399-U1601C-168R-1"	"0.0"	"139.0"	"828.100"	"828.795"	"829.490"	"828.1"	"828.795"	"829.49"	""	"1, 2, 3, 4, 5"	""	"This section is harzburgite with a central interval of orthopyroxene-bearing dunite. Trace chromium spinel is found throughout."	"Highly serpentinized harzburgite and dunite. Bastite is mostly green and locally grey to black or red. Mesh is black and brown.  Spinel is fresh. In addition to serpentine, and serpentine-magnetite veins, this serpentinite contains 3 amphibole-chlorite veins."	"protogranular serp harz and dunite, reg mesh"	
"399"	"U1601"	"C"	"168"	"R"	"2"	""	"399-U1601C-168R-2"	"0.0"	"140.0"	"829.490"	"830.190"	"830.890"	"829.49"	"830.19"	"830.89"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Orthopyroxene-bearing dunite down to 69 cm.  The central interval is oxide and disseminated-oxide gabbro. The base is harzburgite with 10% orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite and highly deformed and variably altered oxide- and Ol-bearing gabbro. Bastite is green to black near the contact with gabbro. Mesh is brown and black. Spinel looks fresh. Peridotite is cut by two hydrothermally altered magmatic veins with a red-brown stain. The extent of alteration increases toward lower serpentinite contact. Abundant oxide and minor sulfide minerals form a network of veins in the gabbro mylonite (pieces 6 and 8). They are cut by a set of talc-carbonate veins that mostly occur in the most altered lower part of the gabbro. Serpentinite contains serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins. Picrolite veins cut through the magmatic veins."	"protogranular serp harz, mylonitic oxide gabbro, protomylonitic gabbro, protogranular weakly foliated harzburgie"	
"399"	"U1601"	"C"	"168"	"R"	"3"	""	"399-U1601C-168R-3"	"0.0"	"69.0"	"830.890"	"831.235"	"831.580"	"830.89"	"831.235"	"831.58"	""	"1, 2, 3, 4, 5"	""	"This section is harzburgite with 10% orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by one hydrothermally altered magmatic vein composed of clinopyroxene, plagioclase, secondary plagioclase, and chlorite. Bastite is green to black. The mesh is black and locally green. Spinel looks fresh. The serpentinite contains a network of serpentine-magnetite veins forming mesh, a network of white fibrous to massive chrysotile veins, and massive picrolite veins. The latter veins cut through the magmatic veins."	"protogranular serp harz with weakly foliated mesh"	
"399"	"U1601"	"C"	"169"	"R"	"1"	""	"399-U1601C-169R-1"	"0.0"	"80.0"	"833.000"	"833.400"	"833.800"	"833"	"833.4"	"833.8"	""	"1, 2, 3"	""	"This section is harzburgite with 18% orthopyroxene and trace chromium spinel and clinopyroxene."	"Highly serpentinized harzburgite. Bastite is green to black. The mesh is black and grey. Spinel looks fresh. The serpentinite contains a network of serpentine-magnetite veins forming mesh and a network of white fibrous to massive chrysotile veins."	"serp harz with patchy regular mesh"	
"399"	"U1601"	"C"	"169"	"R"	"2"	""	"399-U1601C-169R-2"	"0.0"	"142.0"	"833.800"	"834.510"	"835.220"	"833.8"	"834.51"	"835.22"	""	"1, 2, 3"	""	"This section is harzburgite with 15% orthopyroxene and trace chromium spinel and clinopyroxene, grading to orthopyroxene-bearing dunite near gabbroic veins. There are two gabbroic intervals; one is medium grained and cuts through between 18 and 19.5 cm; the second is coarse grained and cuts the section between 118 and 122 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by three hydrothermally altered magmatic veins composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Bastite is black, grey, and green. The mesh is black, brown, and grey. Spinel looks fresh. The serpentinite contains a network of serpentine-magnetite veins forming mesh, a network of white fibrous to massive chrysotile veins, and massive picrolite veins. The latter cut through magmatic veins."	"serpentinized harzburgite with patchy regular mesh, dunite, magmatic veins, pachy wekly foliated ,mesh"	
"399"	"U1601"	"C"	"169"	"R"	"3"	""	"399-U1601C-169R-3"	"0.0"	"140.0"	"835.220"	"835.920"	"836.620"	"835.22"	"835.92"	"836.62"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is harzburgite with 12 % granular orthopyroxene and trace chromium spinel. Some orthopyroxene are large (up to 13 mm)."	"Highly serpentinized harzburgite. Coarse fresh pyroxene.  Bastite is green and black, grey. The mesh is grey and black. Spinel looks fresh. The serpentinite contains a network of serpentine-magnetite veins forming mesh, a network of white fibrous to massive chrysotile veins, and a network of massive picrolite veins."	"protogranular serp harz, reg mesh"	
"399"	"U1601"	"C"	"169"	"R"	"4"	""	"399-U1601C-169R-4"	"0.0"	"73.0"	"836.620"	"836.985"	"837.350"	"836.62"	"836.985"	"837.35"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is harzburgite with 10 % granular orthopyroxene and trace chromium spinel. Some orthopyroxene are large (up to 13 mm)."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by one hydrothermally altered magmatic vein composed of clinopyroxene (brown stain), plagioclase, secondary plagioclase, prehnite, and chlorite. Bastite is black to green. The mesh is black to grey. Spinel looks fresh. The serpentinite contains a network of serpentine-magnetite veins forming mesh, a network of white fibrous to massive chrysotile veins, and massive picrolite veins."	"porphyroclastic (0deg) serp harz, weak mesh (0deg)"	
"399"	"U1601"	"C"	"170"	"R"	"1"	""	"399-U1601C-170R-1"	"0.0"	"128.5"	"837.800"	"838.442"	"839.085"	"837.8"	"838.442"	"839.085"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"The upper portion of the section is harzburgite like that in the overlying section. The lower 27 cm is medium-grained granular gabbro. The first two pieces are fine-grained and mylonitic, whereas the last is coarse-grained."	"Highly serpentinized Opx-bearing dunite/harzburgie and highly altered gabbro. The gabbro is cut by a set of amphibole, chlorite, and zeolite veins. Bastite is black to grey to green. Mesh is grey to black to brown to green. The greenish mesh proportion increases towards the gabbro. The serpentinite contains a network of serpentine-magnetite veins forming mesh and a network of white fibrous to massive chrysotile veins."	"protogranular to porphyroclastic (0deg) serp harz, reg mesh, gabbro mylonite interval"	
"399"	"U1601"	"C"	"171"	"R"	"1"	""	"399-U1601C-171R-1"	"0.0"	"148.0"	"842.700"	"843.440"	"844.180"	"842.7"	"843.44"	"844.18"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"This section consists of a variety of intrusive rocks. The upper 35 cm has medium grained gabbro and hornblende diorite domains. The interval from 35 to 51 cm is diabase. A medium-grained granular gabbro is at the base of the section. It is deformed at 82-103cm, and pyroxenes are partially altered to amphibole."	"Moderately to highly altered gabbro, mylonitic gabbro, and oxide gabbro containing amphibole and prehnite-carbonate veins. Mylonite gabbro shows amphibolite facies alteration. Gabbro and oxide-gabbro show more prominent low-temperature alteration than mylonite gabbro."	"unoriented peices of gabbroic rocks and diabase. oxide gabbro is protomylonitic"	
"399"	"U1601"	"C"	"171"	"R"	"2"	""	"399-U1601C-171R-2"	"0.0"	"135.0"	"844.180"	"844.855"	"845.530"	"844.18"	"844.855"	"845.53"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The uppermost 31 cm are a continuation of the oxide gabbro from the overlying section. It is bounded by orthopyroxene-bearing dunite, with harzburgite (12% orthopyroxene, trace chromium spinel) below 85 cm."	"Highly serpentinized Opx-bearing dunite and moderately altered coarse-grained oxide-bearing gabbro (0-30 cm). The mesh is grey to black. Bastite is black and green. Spinel is fresh. Serpentine and serpentine-magnetite veins in serpentinite. Amphibole, chlorite, prehnite-carbonate, and zeolite veins in gabbroic rocks."	"coarse isotropic fractured ox-gabbro above protogranular serp harz, reg mesh"	
"399"	"U1601"	"C"	"171"	"R"	"3"	""	"399-U1601C-171R-3"	"0.0"	"70.0"	"845.530"	"845.880"	"846.230"	"845.53"	"845.88"	"846.23"	""	"1, 2, 3, 4"	""	"This section is entirely harzburgite with an average of 13% orthopyroxene and trace chromium spinel. The orthopyroxene is more granular than it is interstitial."	"Highly serpentinized harzburgite and Opx-bearing and Opx-free dunite. Mesh is grey to black, and green. Mesh becomes greenish in the dunite. Bastite is black, grey, and green. Spinel is fresh. he serpentinite contains a network of serpentine-magnetite veins forming mesh, a set of white fibrous to massive chrysotile veins, and one composite chrysotile-picrolite vein."	"protogranular to porphyroclastic (0deg) serp harz, reg mesh, gabbro mylonite interval"	
"399"	"U1601"	"C"	"172"	"R"	"1"	""	"399-U1601C-172R-1"	"0.0"	"151.0"	"847.500"	"848.255"	"849.010"	"847.5"	"848.255"	"849.01"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The upper 82.5 cm of this core is orthopyroxene-bearing dunite  with some orthopyroxene between 25-45 cm, and with mm-wide gabbroic impregnations marked by white plagioclase and red (oxidised) pyroxene at 72-82 cm. Coarse-grained, granular oxide gabbro with grain size increasing away from the contact with peridotite above is between 82.5 and 19 cm. Below this is a troctolitic gabbro with anhedral, equant olivine and plagioclase and about 10% clinopyroxene."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein composed of brown stained Cpx and secondary Plag. Variably altered coarse-grained oxide-bearing gabbro and troctolite. Mesh is grey to black, and locally green. Bastite is black and brown. Spinel is fresh. Serpentine and serpentine-magnetite veins in serpentinite."	"dunite and protogranular serp harz, reg to weak mesh (25deg), ox-gabbro-troctolite with thin mylonite pebble, unoriented."	
"399"	"U1601"	"C"	"172"	"R"	"2"	""	"399-U1601C-172R-2"	"0.0"	"140.5"	"849.010"	"849.712"	"850.415"	"849.01"	"849.712"	"850.415"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is made up entirely of gabbroic rocks. The top 67 cm is mylonitic, oxide and oxide-bearing gabbros. Troctolitic olivine gabbro makes up the section between 67 and 129 cm. Oxide-bearing gabbro returns beneath 129 cm."	"Variably altered and deformed Ol- and oxide-bearing gabbro and troctolite. Mesh texture after  is black and contains sulfide. Talc-carbonate-prehnite and amphibole veins. Sulfide after olivine is present close to the talc-carbonate-prehnite veins."	"troctolite protomylonite cut by a gabbro protomylonite cut by a diabase"	
"399"	"U1601"	"C"	"172"	"R"	"3"	""	"399-U1601C-172R-3"	"0.0"	"65.0"	"850.415"	"850.740"	"851.065"	"850.415"	"850.74"	"851.065"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"The top 43 cm is the continuous of the previous olivine gabbro, with the same anhredral, granular texture, but with a higher proportion of plagioclase and an increased grain size. The bottom is oxide-bearing gabbro, here medium-grained and more equigranular."	"Variably altered and deformed Ol- and oxide-bearing gabbro and troctolite (top of the section). The mesh texture after olivine is black and contains sulfides in the troctolite. Some disseminated sulfides occur in the gabbro in the lower part of the section. The gabbro is cut by one sulfide vein, a set of carbonate veins, and talc-carbonate-chlorite-prehnite-sulfide veins that are up to 9 mm wide."	"troctolite with weak magmatic fabric and weakly foliated gabbro"	
"399"	"U1601"	"C"	"173"	"R"	"1"	""	"399-U1601C-173R-1"	"0.0"	"148.0"	"852.400"	"853.140"	"853.880"	"852.4"	"853.14"	"853.88"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The upper 3 cm are orthopyroxene-bearing gabbro. A variety of medium grained and granular gabbroic rocks make up the rest of the section:  gabbro from 3 to 75 cm; olivine gabbro from 75 to 102 cm; oxide gabbro between 102 and 124 cm; and olivine gabbro below 124 cm."	"Variably altered gabbro and highly serpentinized Opx-bearing dunite. The gabbro contains oxide minerals but it is uncertain whether they are of primary or secondary origin. Mesh is black and brown. Bastite is grey and black. Serpentine and serpentine-magnetite veins in serpentinite."	"isoroptric gabbro with felsic melt percolation "	
"399"	"U1601"	"C"	"173"	"R"	"2"	""	"399-U1601C-173R-2"	"0.0"	"148.0"	"853.880"	"854.620"	"855.360"	"853.88"	"854.62"	"855.36"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This section is mostly intrusive with some intermingled peridotites. From 0 to 49 cm, most of the section is coarse-grained gabbro with a minor proportion of orthopyroxene-bearing dunite. Diabase cuts the section between 49 and 58 cm. The diabase is underlain by coarse-grained gabbro, followed by harzburgite with minimal orthopyroxene and trace chromium spinel. This harzburgite is cut by a highly altered gabbroic vein."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of clinopyroxene, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Highly altered gabbro containing amphibole and talc-carbonate-prehnite veins. Mesh is black and brown. Bastite is grey and black. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite."	"gabbro mylonite, fractured above harz with gabbro shear zone. undeformed diabase cross cuts mylonite"	
"399"	"U1601"	"C"	"173"	"R"	"3"	""	"399-U1601C-173R-3"	"14.0"	"100.0"	"855.500"	"855.930"	"856.360"	"855.5"	"855.93"	"856.36"	""	"2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is peridotite with orthopyroxene proportions varying between 0 and 10 %, and with trace chromium spinel. This harzburgite is cut by a c. 2 cm highly altered gabbroic vein centered at 66 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of amphibole, secondary plagioclase, prehnite, chlorite, and one pink to light brown mineral. Reddish rim at the contact with the peridotite in one vein. Some tiny magmatic veins branching on the main one display a reddish-brown stain. The mesh is black, brown, and grey. Bastite is grey and black to green. Bastite tends to be black close to the magmatic veins. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"protogranular serp harz, patchy reg mesh, with dunite interval"	
"399"	"U1601"	"C"	"174"	"R"	"1"	""	"399-U1601C-174R-1"	"0.0"	"150.0"	"857.200"	"857.950"	"858.700"	"857.2"	"857.95"	"858.7"	""	"1, 2, 3, 4, 5"	""	"This section is largely harzburgite with 15% granular orthopyroxene and trace chromium spinel. Thin highly altered gabbro veins are centered at 5, 54, 74, 107, and 113 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of plagioclase, brown-stained clinopyroxene, secondary plagioclase, and chlorite. The mesh is black, grey, and green. Greenish patches. Bastite is grey, black, and green. Spinel is fresh. One small piece of gabbro at the top of the section. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"protogranular serp harz, patchy reg to weak (15deg) mesh"	
"399"	"U1601"	"C"	"174"	"R"	"2"	""	"399-U1601C-174R-2"	"0.0"	"150.0"	"858.700"	"859.450"	"860.200"	"858.7"	"859.45"	"860.2"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This section is largely harzburgite with 18% granular and interstitial orthopyroxene and trace chromium spinel and clinopyroxene. Thin highly altered gabbro veins are present near the top and bottom of the section. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of plagioclase, brown-stained clinopyroxene, secondary plagioclase, and chlorite. Mesh is black, grey, and green. Greenish patches. Bastite is grey and black. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"protogranular to weak porphyroclastic (10deg) serp harz, no mesh to weak fol mesh (10deg)"	
"399"	"U1601"	"C"	"174"	"R"	"3"	""	"399-U1601C-174R-3"	"0.0"	"132.0"	"860.200"	"860.860"	"861.520"	"860.2"	"860.86"	"861.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section down to 120 cm is peridotite with orthopyroxene proportions varying between 0 and 10 %, and with trace chromium spinel. A coarse-grained granular gabbro is present beneath 120 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein composed of brown-stained clinopyroxene, secondary plagioclase, and chlorite. Slightly altered gabbro at the bottom of the section (120-138 cm). It is cut by amphibole and chlorite veins. Mesh is black and brown, grey, and green. Greenish mesh is abundant at the top of the section. Bastite is black, grey, and light brown (possibly after clinopyroxene). Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"Protogranular to weakly foliated mantle fabric in serp harz (0-35deg) with no to regular mesh.  Dunite interval with strongly foliated serpentine foliation (25deg)."	
"399"	"U1601"	"C"	"174"	"R"	"4"	""	"399-U1601C-174R-4"	"0.0"	"45.0"	"861.520"	"861.745"	"861.970"	"861.52"	"861.745"	"861.97"	""	"1, 2, 3"	""	"The top 21 cm is opx-bearing dunite with only granular opx continuous from the previous section. The bottom is coarse-grained seriate granular gabbro with grain size decreasing down section."	"Highly serpentinized Opx-bearing dunite at the top of the section that shows black and brown to green-grey mesh texture. The bastites are black, grey and light brown (possibly after clinopyroxene) and spinel looks fresh. The serpentinite is cut by rare fibrous to massive chrysotile veins. The lower half of the section contains moderately altered gabbro that is strongly veined. The veins are chlorite veins, amphibole veins, and prehnite veins that are up to 2 mm wide."	"weakly foliated serpentinized harzburgite to weakly foliated gabbro"	
"399"	"U1601"	"C"	"175"	"R"	"1"	""	"399-U1601C-175R-1"	"0.0"	"126.0"	"862.100"	"862.730"	"863.360"	"862.1"	"862.73"	"863.36"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"The uppermost 24 cm is gabbro continued from the overlying section. Below is an orthopyroxene-bearing dunite then harzburgite with 10% orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein composed of clinopyroxene and secondary plagioclase. Moderately altered and deformed gabbro at the top of the section (0-22 cm) cut by talc-carbonate veins. The mesh is black, brown, and grey. Bastite is black and grey. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"gabbro with protomylonite above porphyroclastic to protogranular serp harz (25deg) with no mesh to strongly foliated mesh (25deg)"	
"399"	"U1601"	"C"	"175"	"R"	"2"	""	"399-U1601C-175R-2"	"0.0"	"150.0"	"863.360"	"864.110"	"864.860"	"863.36"	"864.11"	"864.86"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Most of the section is harzburgite with 13-15% orthopyroxene and trace clinopyroxene and chromium spinel. Alltered gabbroic veins cut the harzburgite at 26 cm and 97-99 cm."	"Highly serpentinized Opx-bearing dunite and harzburgite; the former is cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, plagioclase, secondary plagioclase, and chlorite. The mesh is black and brown. Bastite is black and green. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite, and hydrothermally altered magmatic veins cut through the serpentinite. Picrolite veins cut through the magmatic veins."	"protogranular serp harz reg mesh"	
"399"	"U1601"	"C"	"175"	"R"	"3"	""	"399-U1601C-175R-3"	"0.0"	"147.0"	"864.860"	"865.595"	"866.330"	"864.86"	"865.595"	"866.33"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Harzburgite with 13 % orthopyroxene grading down to dunite with c 6 % orthopyroxene. Trace chromium spinel is throughout the peridotites. A thin granular gabbro vein cuts the section at 33 cm, and then nearly vertically from 74 cm to 100 cm. A highly deformed gabbro vein cuts the section between 125 and 135 cm."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Mesh is black, brown, green, and white. Green-white mesh forms patches. Bastite is black and green. Serpentine, serpentine-magnetite veins, and hydrothermally altered magmatic veins in serpentinite. Picrolite veins cut through the magmatic veins. One gabbro vein is crosscut by amphibole and talc-carbonate veins."	"protogranular to porphyroclastic serp har (5deg), no mesh to weakly foliated mesh (5deg)"	
"399"	"U1601"	"C"	"176"	"R"	"1"	""	"399-U1601C-176R-1"	"0.0"	"112.0"	"866.900"	"867.460"	"868.020"	"866.9"	"867.46"	"868.02"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The uppermost 24 cm of this section is orthopyroxene-bearing dunite, cut by a thin vein of highly altered gabbro at 8 cm. The rest of the section is coarse-grained oxide gabbro (24-48 cm) and oxide-bearing gabbro (48-100 cm)."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, plagioclase, amphibole, secondary plagioclase, prehnite, and chlorite. Moderately altered and deformed gabbro containing oxide-sulfide veins parallel to the fabric of the rock. The primary or secondary origin of oxides is not constrained. The gabbro is cut by talc-carbonate or sulfate veins and zeolite veins. The mesh is black. Bastite is black. Spinel is fresh. Serpentine, serpentine-magnetite veins, and hydrothermally altered magmatic veins in serpentinite. Picrolite veins cut through the magmatic veins."	"protogranular serp harz above protomylonitic gabbro and oxide gabbro"	
"399"	"U1601"	"C"	"176"	"R"	"2"	""	"399-U1601C-176R-2"	"0.0"	"106.0"	"868.020"	"868.550"	"869.080"	"868.02"	"868.55"	"869.08"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The oxide bearing gabbro from the overlying section continues for the first 7 cm of this section. Most of the rest of the section is mostly coarse-grained gabbro, with an interval of medium grained, disseminated-oxide gabbro between 43 and 80 cm."	"Variably altered Ol-bearing gabbro. Olivine contains sulfides. The gabbro is cut by chlorite, amphibole, zeolite, prehnite, and carbonate or sulfates veins."	"gabbro protomylonite above serp harz above gabbro cataclasite and fault breccia. "	
"399"	"U1601"	"C"	"177"	"R"	"1"	""	"399-U1601C-177R-1"	"0.0"	"133.5"	"871.800"	"872.467"	"873.135"	"871.8"	"872.467"	"873.135"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The top 50 cm is divided between highly altered medium-grained gabbro and harzburgite with 10-12 % orthopyroxene and trace chromium spinel. Below are a series of gabbroic rocks including mixed microgabbro, troctolite, and amphibolitized gabbro between 50 and 95 cm. Beneath 95 cm are domains of a coarse grained gabbro and a mylonitized gabbro."	"Variably altered Ol-bearing gabbro and highly serpentinized Opx-bearing dunite. At the contact with the serpentinite, the gabbro is highly altered and displays a green-to-grey alteration. Gabbro is cut by a network of sulfate veins that do not propagate in the serpentinite. Gabbro is also cut by talc, carbonate-sulfide, and zeolite veins. Mesh is brown and black. Bastite is black. Spinel is fresh. Serpentine, serpentine-magnetite veins in serpentinite."	"Protogranular, no mesh serp harz with gabbro interevals, contact of 90deg. Gabbro is strongly foliated to mylonitic (55-70deg).  Cross cut by shallow to moderately dipping shite and green veins."	
"399"	"U1601"	"C"	"177"	"R"	"2"	""	"399-U1601C-177R-2"	"0.0"	"135.0"	"873.135"	"873.810"	"874.485"	"873.135"	"873.81"	"874.485"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Medium grain granular gabbro makes up the forst 25 cm of this section. Below is harzburgite with 10% orthopyroxene and trace chromium spinel."	"Highly serpentinized harzburgite and Opx-bearing dunite cut by hydrothermally altered magmatic vein made of brown-stained clinopyroxene, secondary plagioclase, and chlorite. The slightly altered Ol-bearing gabbro is cut by talc and zeolite veins. In the serpentinized harzburgite the mesh is brown to black to grey and the bastites are black, whereas spinel looks fresh. The serpentinite is cut by serpentine-magnetite veins, and hydrothermally altered magmatic veins."	"protomylonitie gabbro above  serp harz protogranular no mesh; from 0 to 40 cross cut by fractures"	
"399"	"U1601"	"C"	"177"	"R"	"3"	""	"399-U1601C-177R-3"	"0.0"	"56.0"	"874.485"	"874.765"	"875.045"	"874.485"	"874.765"	"875.045"	""	"1, 2, 3, 4"	""	"Harzburgite with granular opx continuous from previous section. The bottom contain a few gabbro pebbles."	"Highly serpentinized harzburgite showing a brown, black to green-gray mesh texture and black, bronce to green bastites. The serpentinite mesh texture is cut by a set of fibrous to massive chrysotile veins."	"Protogranular serp harz with regular mesh."	
"399"	"U1601"	"C"	"178"	"R"	"1"	""	"399-U1601C-178R-1"	"0.0"	"150.0"	"876.600"	"877.350"	"878.100"	"876.6"	"877.35"	"878.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"The top 49 cm of this section grades downward from a orthopyroxene-bearing dunite to harzburgite with minimal orthopyroxene and trace chromium spinel. Immediately below is an olivine-bearing gabbro with a chilled margin and acoarser-grained center. A diorite that may represent a metamorphosed gabbro is present from 59-62 cm. Below 62 cm are a series of gabbros. The upper and lower portions are medium-grained, the center is coarse-grained."	"Variably altered olivine-bearing gabbro and highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic vein made of brown-stained clinopyroxene, secondary plagioclase, and chlorite. At the contact with serpentinite, the gabbro appears greenish. The mesh is black and brown, and at the contact with gabbro, the mesh is brown. Bastite is black to green and locally has a brown corona. Spinel is fresh. Serpentine-magnetite veins, chrysotile and hydrothermally altered magmatic veins occur in the serpentinite. In the gabbro sets of amphibole veins and talc-carbonate-prehnite veins occur."	"porphyroclastic (15deg) to protogranular serp above altered gabbro variably deformed by protomylonitic deformation and later faulting and talc alteration"	
"399"	"U1601"	"C"	"178"	"R"	"2"	""	"399-U1601C-178R-2"	"0.0"	"149.0"	"878.100"	"878.845"	"879.590"	"878.1"	"878.845"	"879.59"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The majority of this section is orthopyroxene-bearing dunite with trace chromium spinel. Millimeter-scale, highly deformed and altered gabbro veins cut this dunite in several places. From 70 cm to the base of the section is coarse-grained and granular gabbro whose primary features are obscured by fracturing and alteration. "	"Variably altered and deformed gabbro and highly serpentinized Opx-bearing dunite. Mesh is brown and black. Bastite is black. Serpentine-magnetite veins, chrysotile, carbonate-sulfide, serpentine-sulfide veins in serpentinite; sets of amphibole-chlorite veins and talc-carbonate-prehnite veins in gabbro."	"gabbro mylonite with irregular interfingered contact with harz also mylonitised. serp harz below with contact against lower sections of gabbro mylonite rubble"	
"399"	"U1601"	"C"	"179"	"R"	"1"	""	"399-U1601C-179R-1"	"0.0"	"146.0"	"881.500"	"882.230"	"882.960"	"881.5"	"882.23"	"882.96"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"The top and bottom of this section consist of highly deformed, coarse-grained gabbro. The interval from 4 to 75 cm is a relatively fine-grained olivine gabbro, with grain size decreasing towards the upper and lower contacts. "	"Variably altered and variably deformed Ol-bearing gabbro to troctolite. Greenish alteration is more abundant at the top of the section. Amphibole veins are parallel to and locally cutting the foliation, and talc-carbonate-prehnite veins cut amphibole veins."	"gabbro isotropic undeformed, with foliated and protomylonitic intervals"	
"399"	"U1601"	"C"	"179"	"R"	"2"	""	"399-U1601C-179R-2"	"0.0"	"148.0"	"882.960"	"883.700"	"884.440"	"882.96"	"883.7"	"884.44"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is primarily disseminated oxide gabbro that was originally coarse-grained, but was comminuted by deformation. Relict large cpx, plag grain size and overal texture obscured. Orthopyroxene may be present in this gabbro. Approximately 5% of this section consists of dunite domains"	"Highly altered and deformed gabbro, and a minor amount of serpentinized peridotite. Mesh is brown-black, and bastite is black. The extent of alteration in gabbro increases toward the contact with serpentinite. Plagioclase is more extensively altered than Cpx. Serpentine-magnetite veins and chrysotile veins in serpentinite; a network of carbonate + white mineral veins and a set of talc-carbonate veins in gabbro."	"gabbro with sheared contact mylonitic against harz. protomylonitic sections offset by lkate faults"	
"399"	"U1601"	"C"	"179"	"R"	"3"	""	"399-U1601C-179R-3"	"0.0"	"39.0"	"884.440"	"884.635"	"884.830"	"884.44"	"884.635"	"884.83"	""	""	""	"This section is variably deformed, originally coarse-grained disseminated oxide gabbro."	"Highly altered and deformed gabbro cut by a network of prehnite-carbonate veins."	"protomylonite gabbro offset by white veins"	
"399"	"U1601"	"C"	"180"	"R"	"1"	""	"399-U1601C-180R-1"	"0.0"	"146.0"	"886.300"	"887.030"	"887.760"	"886.3"	"887.03"	"887.76"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"The top 42 cm consists of a variably deformed, coarse-grained orthopyroxene-bearing gabbro. The interval between 42 and 127 cm is orthopyroxene-bearing dunite with trace chromium spinel, cut by minor veins of highly altered gabbro and gabbronorite.  Olivine-bearing gabbro makes up the section below 127 cm. It is coarse grained, and its olivine was likely derived from the adjacent peridotite."	"Highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of brown stained Cpx, amphibole, plagioclase, secondary plagioclase, chlorite, and prehnite in variable volume proportions. Variably altered Ol-bearing gabbro. At the contact with serpentinite, the alteration degree of gabbro increases, showing green and white colors and abundant prehnite. Mesh is brown and black. Bastite is black and locally green. Spinel is fresh. Serpentine-magnetite veins, chrysotile, picrolite cutting hydrothermally altered magmatic veins in serpentinite; a network of carbonate + possibly quartz veins and a set of talc-carbonate-prehnite veins in gabbro."	"isotropic gabbro in contact with serpentinized protogranular harzburgite with a weak mantle fabric"	
"399"	"U1601"	"C"	"180"	"R"	"2"	""	"399-U1601C-180R-2"	"0.0"	"145.0"	"887.760"	"888.485"	"889.210"	"887.76"	"888.485"	"889.21"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26"	""	"The olivine bearing gabbro from the overlying section continues down to 109 cm. The portion of the interval below 41 cm has domains of orthopyroxene-bearing dunite with trace chromium spinel. Below 109 cm is a medium-grained, granular to subophitic gabbro. "	"Variably altered gabbroic rocks and highly serpentinized harzburgite. The extent of alteration of gabbroic rocks varies from slight to complete and is highest at the contact with serpentinite. Serpentinized harzburgite shows sulfide mineralization in veins and disseminated in the rock matrix. Spinel is fresh. Serpentine-magnetite and serpentine-sulfide veins, picrolite, carbonate, and carbonate-sulfide veins in serpentinite; a network of talc-carbonate veins and a set of zeolite veins in gabbro."	"undeformed mafic rocks in contact with harzburgite"	
"399"	"U1601"	"C"	"180"	"R"	"3"	""	"399-U1601C-180R-3"	"0.0"	"33.0"	"889.210"	"889.375"	"889.540"	"889.21"	"889.375"	"889.54"	""	"1, 2"	""	"This section consists mostly of granular gabbro with harzburgite interval."	"Highly altered Ol-bearing gabbro that is cut by a network of carbonate-prehnite-talc veins with one vein up to 8 mm wide. The lower part of the section shows greenish alteration (between 24-33 cm). In the middle of the section (18-23 cm) serpentinized harzburgite occurs that has a black to black-brown mesh and sulfides occurring in the mesh."	"strongly foliated serp-harz sandwhiched between two gabbroic dikes"	
"399"	"U1601"	"C"	"181"	"R"	"1"	""	"399-U1601C-181R-1"	"0.0"	"144.0"	"891.200"	"891.920"	"892.640"	"891.2"	"891.92"	"892.64"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is entirely harzburgite averaging 18% orthopyroxene, with trace chromium spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. Mesh is brown-black and becomes grey down section. Bastite is mostly green and locally black. The magmatic veins are composed of chlorite and amphibole, secondary plagioclase. Some of the bastite contains serpentine and talc but most are composed of serpentine only. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinized harzburgite."	"protogranular harzburgite with regular mesh"	
"399"	"U1601"	"C"	"181"	"R"	"2"	""	"399-U1601C-181R-2"	"0.0"	"150.0"	"892.640"	"893.390"	"894.140"	"892.64"	"893.39"	"894.14"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section consists mostly of harzburgite averaging 15% orthopyroxene, with trace chromium spinel. It is cut by diffuse gabbroic veins at c. 13, 28, 59, and 148 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite. Both are cut by hydrothermally altered magmatic veins composed of Cpx, plagioclase, secondary, plagioclase, amphibole, chlorite, and prehnite. Mesh is black-brown and locally grey. Bastite is mostly green and grey to black. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinized harzburgite and Opx-bearing dunite."	"protogranular serpentinized harzburgite with patchy regular mesh and horizontal little white veins"	
"399"	"U1601"	"C"	"181"	"R"	"3"	""	"399-U1601C-181R-3"	"0.0"	"143.0"	"894.140"	"894.855"	"895.570"	"894.14"	"894.855"	"895.57"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27"	""	"Harzburgite cut by diffuse gabbro veins is at the top down to 31 cm. Below is a coarse-grained gabbro that is partially amphibolitized. The section terminates in a pebble of opx-bearing dunite."	"Moderately altered Ol-bearing gabbro and highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of amphibole, plagioclase, secondary plagioclase, chlorite, prehnite, and a pink mineral. Bastite is green. Mesh is brown and black. Sulfides are disseminated in the gabbro, probably replacing olivine. Olivine in peridotite close to the contact is quite fresh overall. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinized peridotite. Talc-carbonate-prehnite and carbonate-white minerals cut the gabbro."	"serpentinized harzburgite with gabbro which is locally protomylonitic"	
"399"	"U1601"	"C"	"182"	"R"	"1"	""	"399-U1601C-182R-1"	"0.0"	"149.0"	"896.000"	"896.745"	"897.490"	"896"	"896.745"	"897.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is harzburgite with 14% orthopyroxene and trace clinopyroxene and chromium spinel. "	"Highly serpentinized Opx-bearing dunite cut by magmatic vein composed of Cpx, plagioclase, secondary plagioclase, chlorite, and prehnite. Mesh is black-brown. Bastite is black to green. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite."	"protogranular to wekly porphyroclastic serpentinized harzburgite with no or regular mesh"	
"399"	"U1601"	"C"	"182"	"R"	"2"	""	"399-U1601C-182R-2"	"0.0"	"150.0"	"897.500"	"898.250"	"899.000"	"897.5"	"898.25"	"899"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"The upper 17 cm and lowermost 68 cm are mostly harzburgite with 14% orthopyroxene and trace clinopyroxene and chromium spinel. The central portion is cut by orthopyroxene-bearing dunite with trace chromium spinel. This portion of the section is cut by gabbroic veins centered at c. 31, 43, and 46 cm."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by magmatic vein composed of Cpx, plagioclase, secondary plagioclase, amphibole, chlorite, and prehnite. Mesh is black-brown. Bastite is mostly green and locally grey, black (where it is close to the magmatic vein), or brown. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite."	"weakly porphyroclastic serpentinized harzburgite with horizontal or shallowly inclined mantle fabric and regular mesh, rodingite vein"	
"399"	"U1601"	"C"	"182"	"R"	"3"	""	"399-U1601C-182R-3"	"0.0"	"145.0"	"899.000"	"899.725"	"900.450"	"899"	"899.725"	"900.45"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The upper 110 cm is harzburgite with 11% orthopyroxene and trace clinopyroxene and chromium spinel. Below is a coarse-grained, granular gabbro with some olivine potentially derived from the peridotite."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic vein. Moderately altered gabbro. The altered magmatic vein is composed of secondary plagioclase and chlorite. Mesh is black-brown. Bastite is black and grey. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. Gabbro contains zeolite and prehnite chlorite veins."	"protogranular serpentinized harzburgite without mesh"	
"399"	"U1601"	"C"	"182"	"R"	"4"	""	"399-U1601C-182R-4"	"0.0"	"24.0"	"900.450"	"900.570"	"900.690"	"900.45"	"900.57"	"900.69"	""	"1, 2"	""	"The top 17 cm is opx-bearing dunite. Below is coarse-grained, granular gabbro with some olivine (potentially derived from peridotite)."	"Highly serpentinized, opx-bearing dunite and Ol-bearing gabbro at the bottom of the section. The serpentinized dunite contains a network of fibrous to massive chyrsotile veins and a set of carbonate veins that cut the serpentinite mesh texture. The gabbro is comprised of clinopyroxene, plagioclase, secondary plagioclase, prehnite, chlorite, and amphibole. The gabbro is cut by zeolite and carbonate-prehnite-chlorite-talc veins and contains disseminated sulfides."	"Protogranular serp harz with no mesh cut by little white veins (10deg) and isotropic gabbro."	
"399"	"U1601"	"C"	"183"	"R"	"1"	""	"399-U1601C-183R-1"	"0.0"	"143.0"	"900.900"	"901.615"	"902.330"	"900.9"	"901.615"	"902.33"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"Most of this section is harzburgite with spinel trails and both granular and interstitial orthopyroxene (c. 10%). Parts of the harzburgite are relatively fresh. It is cut by medium-grained granular gabbro forming both discrete (1-7cm, 84-93cm) and diffuse (105-107cm, 119-126cm) veins through the host harzburgite."	"Highly serpentinized Opx-bearing dunite/harzburgite cut by hydrothermally altered magmatic veins. Moderately altered gabbro at the top of the section. The altered magmatic veins are composed of plagioclase, secondary plagioclase, Cpx, amphibole, chlorite, and prehnite. Mesh is black-brown. Bastite is mostly green and locally grey. Black corona around bastite. Olivine is fresh next to bastite. Spinel is fresh. Secondary sulfide associated with Amp in gabbro and magmatic veins."	"protogranular serpentinized harzburgite without mesh and contact with gabbro in 0-10cm"	
"399"	"U1601"	"C"	"183"	"R"	"2"	""	"399-U1601C-183R-2"	"0.0"	"143.0"	"902.330"	"903.045"	"903.760"	"902.33"	"903.045"	"903.76"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Gabbroic pebbles are at the top and bottom of the section. The rest is harzburgite with both granular and interstitial orthopyroxene (12%) and trace chromium spinel. "	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic vein. The top and bottom of the section consist of moderately altered gabbro. The altered magmatic vein is composed of secondary plagioclase and chlorite. Mesh is black-brown. Bastite is black and locally green. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. Gabbro contains prehnite-chlorite-zoisite and chlorite veins."	"isotropic gabbro in 0-10, protogrnaular serpentinized harxburgite with inclined to steeply dipping weak serpentine mesh"	
"399"	"U1601"	"C"	"184"	"R"	"1"	""	"399-U1601C-184R-1"	"0.0"	"150.0"	"905.700"	"906.450"	"907.200"	"905.7"	"906.45"	"907.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"This section is coarse-grained, granular gabbro, which is variably deformed, obscuring its primary properties. Oxide diorite domains are present throughout the gabbro unit, where clinopyroxene is commonly replaced by black amphibole plus Fe-Ti oxides."	"Variably altered oxide gabbro. Sulfide minerals are associated with amphibole after clinopyroxene. Gabbro is cut by talc-carbonate veins and veins composed of carbonate and an unidentified white mineral."	"undeformed, protomylonitic and mylonitic gabbro rubble with locally brittle overprint by fracturing"	
"399"	"U1601"	"C"	"184"	"R"	"2"	""	"399-U1601C-184R-2"	"0.0"	"150.0"	"907.200"	"907.950"	"908.700"	"907.2"	"907.95"	"908.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28, 29, 30"	""	"This section is coarse-grained, granular gabbro, which is variably deformed, obscuring its primary properties. Oxide diorite domains are present particularly at the top of the section, where clinopyroxene is commonly replaced by black amphibole plus Fe-Ti oxides."	"Altered olivine-bearing gabbro containing oxides of likely secondary origin. Sulfides associated with amphibole after Opx and possibly also after olivine. Gabbro contains talc-carbonate veins and veins composed of carbonate and an unidentified white mineral."	"isotropic gabbro, 0-5cm cataclastic"	
"399"	"U1601"	"C"	"185"	"R"	"1"	""	"399-U1601C-185R-1"	"0.0"	"142.0"	"910.600"	"911.310"	"912.020"	"910.6"	"911.31"	"912.02"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"The top 54 cm is coarse-grained granular gabbro. The rest is harzburgite with 11% mostly granular orthopyroxene and trace chromium spinel."	"Highly serpentinized Opx-bearing dunite and slightly altered Ol-bearing gabbro. Mesh is black-brown and locally grey. Bastite is green and grey. The extent of serpentinization is locally variable with relict olivine close to Opx/bastite. Quartz(?)-prehnite veins cut the gabbro. Serpentine and serpentine-magnetite veins occur in serpentinite."	"fractured gabbro, weakly porphyroclastic serpentinized harzburgite horizontal with horiznotal weakly foliated mesh"	
"399"	"U1601"	"C"	"185"	"R"	"2"	""	"399-U1601C-185R-2"	"0.0"	"146.0"	"912.020"	"912.750"	"913.480"	"912.02"	"912.75"	"913.48"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is orthopyroxene-bearing dunite grading downward to harzburite averaging 13% orthopyroxene and trace chromium spinel. Small highly altered gabbroic veins cut the perdotites centered at 3, 74, and 120 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh is black-brown. Bastite is black, green, and light brown (possibly after Cpx). Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. Magmatic veins are also cut by picrolite veins."	"protogranulr to horizontal porphyroclastic serpentinized harzburgite with a horizontal wekly foliated mesh"	
"399"	"U1601"	"C"	"185"	"R"	"3"	""	"399-U1601C-185R-3"	"0.0"	"146.0"	"913.480"	"914.210"	"914.940"	"913.48"	"914.21"	"914.94"	""	"1, 2, 3, 4, 5"	""	"This section is harzburgite with about 15% orthopyroxene and trace chromium spinel. The orthopyroxene is containing both granular and interstitial. Some granular grains are particularly rounded. A diffuse gabbroic patch is at c. 132 cm."	"Highly and variably serpentinized harzburgite cut by hydrothermally altered magmatic vein made of chlorite and amphibole. The extent of serpentinization is variable. Relict olivine is locally present. Mesh is black-brown. Bastite is green and black. Spinel is variably altered to chlorite. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite."	"protogranular serpentinized harzburgite, weakly foliated horizontal mesh 0-70,regular mesh 70-125, moderate shallowly dipping mesh mesh 125-147"	
"399"	"U1601"	"C"	"185"	"R"	"4"	""	"399-U1601C-185R-4"	"0.0"	"25.0"	"914.940"	"915.065"	"915.190"	"914.94"	"915.065"	"915.19"	""	"1, 2"	""	"This section mostly consists of harzburgite containing both granular and interstitial opx with highly altered gabbro domain. "	"Variably serpentinized harzburgite cut by hydrothermally altered magmatic vein in pieces 1 and 2. The extent of serpentinization is variable, leaving olivine relicts next to the bastites. The serpentinite mesh texture is cut by a set of subparallel, fibrous to massive chrysotile veins. The hydrothermally altered magmatic vein is made of chlorite and amphibole and is up to 10 mm wide."	"Protogranular to weakly foliated porphyroclastic (20deg) mantle fabric with no to weakly foliated mesh (15deg) cut by little white veins (15-20deg)."	
"399"	"U1601"	"C"	"186"	"R"	"1"	""	"399-U1601C-186R-1"	"0.0"	"145.0"	"915.400"	"916.125"	"916.850"	"915.4"	"916.125"	"916.85"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with about 10% orthopyroxene and trace chromium spinel. The orthopyroxene is both granular and interstitial. Highly altered gabbroic veins cut the section centered at 17 cm and 54 cm"	"Highly serpentinized harzburgite and Opx-bearing dunite cut by hydrothermally altered magmatic vein made of clinopyroxene, plagioclase, secondary plagioclase, and chlorite. Opx content is variable. The mesh is black-brown and grey. Bastite is black, green, grey, and light brown (possibly after Cpx). Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. Magmatic veins are cut by picrolite veins."	"protogranular to wekly porphyroclastic serpentinized harzburgite with a horizontal to shallowly dipping mantle fabric"	
"399"	"U1601"	"C"	"186"	"R"	"2"	""	"399-U1601C-186R-2"	"0.0"	"146.0"	"916.850"	"917.580"	"918.310"	"916.85"	"917.58"	"918.31"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is mainly harzburgite with minimal orthopyroxene. The orthopyroxene is both granular and interstitial. The interval between 114 and 125 is orthopyroxene-bearing dunite. Chromium spinel is in trace amounts throughout."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein made of chlorite, clinopyroxene, amphibole, and prehnite. Mesh is black-brown. Bastite is green and minor black. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. The magmatic vein is cut by picrolite veins."	"weakly porphyroclastic to protogranular horizontal serpentinized harzburgite, with regular to moderately foliated mesh, dunite with a strong mesh foliation dipping shallow, faulted magnetite vein with a reverse sense of shear, and another fault with strike-slip slickenfibres"	
"399"	"U1601"	"C"	"186"	"R"	"3"	""	"399-U1601C-186R-3"	"0.0"	"150.0"	"918.310"	"919.060"	"919.810"	"918.31"	"919.06"	"919.81"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is harzburgite with minimal orthopyroxene and trace chromium spinel. The orthopyroxene is both granular and interstitial."	"Highly serpentinized harzburgite cut by a hydrothermally altered magmatic vein made of brown-stained clinopyroxene. Mesh is black-brown. Bastite is green and black. Spinel is variably altered to chlorite. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. The magmatic vein is cut by picrolite veins."	"weakly porphyclastic horizontal serpentinized harzburgite with a horizontal weakly foliated mesh"	
"399"	"U1601"	"C"	"186"	"R"	"4"	""	"399-U1601C-186R-4"	"0.0"	"41.0"	"919.810"	"920.015"	"920.220"	"919.81"	"920.015"	"920.22"	""	"1, 2, 3, 4, 5"	""	"This section is harzburgite with both granular and interstitial opx and trace Cr-spinel. No apparent cpx. Modal opx increased down section."	"Highly serpentinized harzburgite with a mesh that is black-brown and the bastites are green and black. Spinel is variably altered to chlorite. The serpentinite mesh texture is cut by a dense set of subparallel, fibrous to massive chrysotile veins"	"weakly foliated serpentinized harz with regular mesh"	
"399"	"U1601"	"C"	"187"	"R"	"1"	""	"399-U1601C-187R-1"	"0.0"	"140.0"	"920.300"	"921.000"	"921.700"	"920.3"	"921"	"921.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with minimal orthopyroxene and trace chromium spinel. The orthopyroxene is mostly granular."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins made of brown-stained Cpx and other unidentified minerals. The extent of serpentinization is variable. Relicts of olivine are locally associated with bastite/Opx. Mesh is black-brown. Bastite is green and black. Spinel is variably altered to chlorite. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. Magmatic veins are cut by picrolite veins."	"weakly porphyclastic horizontal serpentinized harzburgite with a horizontal weakly foliated mesh"	
"399"	"U1601"	"C"	"187"	"R"	"2"	""	"399-U1601C-187R-2"	"0.0"	"145.0"	"921.700"	"922.425"	"923.150"	"921.7"	"922.425"	"923.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with 13% orthopyroxene and trace chromium spinel. The orthopyroxene is mostly granular."	"Highly serpentinized harzburgite. Mesh is black-brown. Bastite is green and black. Spinel is fresh. Serpentine and serpentine-magnetite cut the serpentinite."	"weakly porphyclastic horizontal serpentinized harzburgite with a horizontal weakly foliated mesh"	
"399"	"U1601"	"C"	"187"	"R"	"3"	""	"399-U1601C-187R-3"	"0.0"	"149.0"	"923.190"	"923.935"	"924.680"	"923.19"	"923.935"	"924.68"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is harzburgite with 12% orthopyroxene and trace chromium spinel and clinopyroxene. The orthopyroxene is both granular and interstitial."	"Highly serpentinized harzburgite cut by one hydrothermally altered magmatic vein made of red-stained clinopyroxene, prehnite, and chlorite. Relicts of olivine are associated with bastite/Opx. Mesh is black-brown. Bastite is mostly green and locally black-brown. Spinel has a yellowish color. Serpentine, serpentine-magnetite, and hydrothermally altered magmatic veins cut the serpentinite. The magmatic vein is cut by picrolite veins."	"Porphyroclastic (0deg) serp harz, weak foliated mesh (0deg)"	
"399"	"U1601"	"C"	"187"	"R"	"4"	""	"399-U1601C-187R-4"	"0.0"	"24.0"	"924.680"	"924.800"	"924.920"	"924.68"	"924.8"	"924.92"	""	"1, 2"	""	"This section is harzburgite with 12% orthopyroxene and trace chromium spinel and clinopyroxene. The orthopyroxene is both granular and interstitial.</span>"	"Highly serpentinized harzburgite with relicts of olivine that are associated with bastite/Opx. The mesh is black-brown and bastites are mostly green and locally black-brown. The serpentinite mesh texture is cut by a set of subparallel, fibrous to massive chrysotile veins."	"strongly foliated serp harz"	
"399"	"U1601"	"C"	"188"	"R"	"1"	""	"399-U1601C-188R-1"	"0.0"	"135.0"	"925.100"	"925.775"	"926.450"	"925.1"	"925.775"	"926.45"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"This section is harzburgite with 15% orthopyroxene and trace chromium spinel and clinopyroxene. The orthopyroxene is both granular and interstitial."	"Highly serpentinized harzburgite cut by two magmatic veins altered to chlorite. Relicts of Ol are associated with bastite/Opx. Mesh is black-brown. Bastite is mostly green and locally grey and black. Spinel is fresh. Serpentine, serpentine-magnetite, and hydrothermally altered possibly magmatic veins cut the serpentinite. Magmatic veins are cut by picrolite veins."	"Porphyroclastic (0deg) serp harz, weak foliated mesh (0deg)"	
"399"	"U1601"	"C"	"188"	"R"	"2"	""	"399-U1601C-188R-2"	"0.0"	"150.0"	"926.450"	"927.200"	"927.950"	"926.45"	"927.2"	"927.95"	""	"01, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This section is harzburgite with 12% orthopyroxene and trace chromium spinel and clinopyroxene down to 45 cm. The orthopyroxene is both granular and interstitial. Below is medium-grained gabbro varying from subophitic to granular in texture. "	"Highly to completely serpentinized harzburgite and slightly altered gabbro. Mesh is black-brown. Bastite is green. Spinel is fresh. Serpentine + magnetite and chrysotile veins are present in serpentinite. Talc + white mineral, amphibole, and zeolite veins are present in gabbro."	"Porphyroclastic (0deg) serp harz, weak foliated mesh (0deg), above isotropic gabbro with vertical fault with sheared margin"	
"399"	"U1601"	"C"	"188"	"R"	"3"	""	"399-U1601C-188R-3"	"0.0"	"97.0"	"927.950"	"928.435"	"928.920"	"927.95"	"928.435"	"928.92"	""	"01, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The medium-grained gabbro from the overlying section continues. Its texture varies from subophitic to granular."	"Slightly altered gabbro. The extent of alteration increases toward veins. Gabbro contains amphibole-chlorite veins and talc-prehnite (-carbonate?) veins."	"isotropic gabbro with grain size variations, green faulted veins"	
"399"	"U1601"	"C"	"189"	"R"	"1"	""	"399-U1601C-189R-1"	"0.0"	"150.0"	"930.000"	"930.750"	"931.500"	"930"	"930.75"	"931.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The medium-grained gabbro from the overlying section continues. Its texture is mostly subophitic but becomes granular beneath 110 cm."	"Moderately altered gabbro. The extent of alteration is highest at the bottom of the section with brecciation. Some of the Cpx along veins have a light brown stain. Amphibole, talc +/- carbonate, and zeolite veins are present in gabbro."	"isotropic gabbro with localised magmatic foliation (35deg). localised fracturing and faulting"	
"399"	"U1601"	"C"	"189"	"R"	"2"	""	"399-U1601C-189R-2"	"0.0"	"144.0"	"931.500"	"932.220"	"932.940"	"931.5"	"932.22"	"932.94"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The medium-grained gabbro with varring grain sizes from the overlying section continues. "	"Moderately and variably altered gabbro with zeolite veins and talc + prehnite + white mineral (carbonate?) veins. The abundance of talc in the veins decreases in the areas where Cpx in gabbro is replaced by amphibole."	"isotropic gabbro. faulted talc veins"	
"399"	"U1601"	"C"	"189"	"R"	"3"	""	"399-U1601C-189R-3"	"0.0"	"131.0"	"932.940"	"933.595"	"934.250"	"932.94"	"933.595"	"934.25"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The section is mostly medium-grained gabbro but has two coarse-grained pieces at 1-9cm and 44-55cm (12mm for cpx and 10mm for plag). It has a diorite pebble at around 56 cm."	"Moderately to highly altered coarse-grained gabbro. The extent of alteration is higher near hydrothermal veins. Cpx has a brown stain. Gabbro contains talc veins, amphibole veins, and zeolite veins."	"isotropic gabbro with localised spo. dark green amp vein cut by green talc vein"	
"399"	"U1601"	"C"	"190"	"R"	"1"	""	"399-U1601C-190R-1"	"0.0"	"148.0"	"934.800"	"935.540"	"936.280"	"934.8"	"935.54"	"936.28"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"An oxide-gabbro pebble is at the top. It is underlain by orthopyroxene-bearing dunite grading downward to harzburgite with about 10% granular and interstitial orthopyroxene. Both peridotites have trace chromium spinel and clinopyroxene."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins composed of brown/red-stained Cpx, chlorite, and secondary plagioclase. Mesh is brown-black and locally grey. Bastite is green and black. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"protogranular to porphyroclastic (25deg) serp harz with reg to weak foliated mesh (25deg)"	
"399"	"U1601"	"C"	"190"	"R"	"2"	""	"399-U1601C-190R-2"	"0.0"	"118.0"	"936.280"	"936.870"	"937.460"	"936.28"	"936.87"	"937.46"	""	"1, 2, 2, 3, 3, 4, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with about 10% granular and interstitial orthopyroxene and trace chromium spinel and clinopyroxene."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of possibly chlorite and amphibole. Mesh is brown to black. Bastite is dark to light green and black. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"protogranular to porphyroclastic (20deg) serp harz with weak foliated mesh (20deg)"	
"399"	"U1601"	"C"	"190"	"R"	"3"	""	"399-U1601C-190R-3"	"0.0"	"95.0"	"937.460"	"937.935"	"938.410"	"937.46"	"937.935"	"938.41"	""	"01, 02, 3, 4, 5, 6, 7, 8, 9"	""	"This section is harzburgite with about 10% granular and interstitial orthopyroxene and trace chromium spinel and clinopyroxene."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of Px (Cpx?) with brown stain, chlorite, and amphibole. Mesh is brown to black. Bastite is dark to light green and black. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"protogranular serp harz reg mesh cut by magnetite veins"	
"399"	"U1601"	"C"	"191"	"R"	"1"	""	"399-U1601C-191R-1"	"0.0"	"138.0"	"939.700"	"940.390"	"941.080"	"939.7"	"940.39"	"941.08"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is mostly harzburgite with about 10% largely granular orthopyroxene and trace chromium spinel and clinopyroxene. A medium-grained granular gabbro forming a discrete vertical vein crosscutting the host harzburgite in the upper 28 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of Cpx, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh is brown to black. Bastite is dark to light green and black. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"protogranular serp harz reg mesh cut by magnetite veins"	
"399"	"U1601"	"C"	"191"	"R"	"2"	""	"399-U1601C-191R-2"	"0.0"	"150.0"	"941.080"	"941.830"	"942.580"	"941.08"	"941.83"	"942.58"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is mostly harzburgite with about 10% largely granular orthopyroxene and trace chromium spinel and clinopyroxene. A medium-grained granular gabbro forming a discrete vertical vein crosscuttis the host harzburgite at c. 28 cm."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of Cpx with locally brown stain, amphibole, plagioclase, secondary plagioclase, prehnite, and chlorite. Mesh is brown to black. Bastite is dark to light green and black. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"protogranular to porphyroclastic (0-25deg) serp harz with reg to weak foliated mesh (0deg)"	
"399"	"U1601"	"C"	"191"	"R"	"3"	""	"399-U1601C-191R-3"	"0.0"	"150.0"	"942.580"	"943.330"	"944.080"	"942.58"	"943.33"	"944.08"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is harzburgite with about 10% largely granular orthopyroxene and trace chromium spinel and clinopyroxene. "	"Highly serpentinized harzburgite. Mesh is brown to black. Bastite is grey, black, and minor green. Spinel is fresh. Mesh-forming serpentine-magnetite, chrysotile, and picrolite veins."	"porphyroclastic (10-20deg) serp harz with no mesh to weak foliated mesh (20-30deg)"	
"399"	"U1601"	"C"	"192"	"R"	"1"	""	"399-U1601C-192R-1"	"0.0"	"146.0"	"944.500"	"945.230"	"945.960"	"944.5"	"945.23"	"945.96"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is orthopyroxene-bearing dunite grading downward to harzburgite with about 12% largely granular orthopyroxene and trace chromium spinel. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of secondary plagioclase, amphibole, brown-stained Cpx, chlorite, and prehnite. Mesh is brown to black, and greenish in patches. Relatively large magnetite veins within mesh in a patch (31-36 cm). Bastite is grey to black and minor green. Spinel is almost fresh but has a small amount of reddish stain. The extent of serpentinization decreases down section. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"porphyroclastic (0deg) serp harz with reg mesh"	
"399"	"U1601"	"C"	"192"	"R"	"2"	""	"399-U1601C-192R-2"	"0.0"	"142.0"	"945.960"	"946.670"	"947.380"	"945.96"	"946.67"	"947.38"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is largely harzburgite with about 11% largely granular orthopyroxene and trace chromium spinel. Pervasively altered diffuse gabbroic veins and patches are prsent at 48-54cm, 111-113cm, 123-124cm. "	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of secondary plagioclase, prehnite, amphibole, chlorite, and Cpx. Mesh is brown to black. Bastite is mostly black and minor green. Spinel is fresh. Relict olivine is more abundant close to magmatic veins. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins."	"porphyroclastic (0deg - varying locally by 5deg) serp harz with no mesh to weak foliated mesh (20-30deg)"	
"399"	"U1601"	"C"	"192"	"R"	"3"	""	"399-U1601C-192R-3"	"0.0"	"125.0"	"947.380"	"948.005"	"948.630"	"947.38"	"948.005"	"948.63"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is largely harzburgite with about 11% largely granular orthopyroxene and trace chromium spinel. "	"Highly serpentinized harzburgite. Mesh is brown to black. Bastite is light green to black. Spinel is fresh. Mesh-forming serpentine-magnetite and chrysotile, some of which form slickensides."	"protogranular to porphyroclastic (10-20deg) serp harz with weak to strong foliated mesh (10-20)"	
"399"	"U1601"	"C"	"193"	"R"	"1"	""	"399-U1601C-193R-1"	"0.0"	"148.0"	"949.400"	"950.140"	"950.880"	"949.4"	"950.14"	"950.88"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"This section has a variably altered gabbroic rocks interspersed with orthopyroxene-bearing dunite with trace chromium spinel from 0-29.5, 79-82, and 92-99 cm. The gabbros above 92 cm are medium grained. Below they are coarse grained. Oxide gabbros are present at 48-52, 99-104, and 131-138 cm."	"Variably altered oxide-bearing gabbro and highly serpentinized Opx-bearing dunite cut by a hydrothermally altered magmatic vein composed of brown-stained Cpx, secondary plagioclase, chlorite, and prehnite. The mesh is black to brown. Bastite is green and white and possibly formed after Cpx. A black corona is present around Opx. Olivine in serpentinite at the contact with gabbro is relatively fresh. Oxide is associated with probably primary sulfide in gabbro. Sulfide inclusions are present in igneous silicates. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins in serpentinite. Amphibole, talc, chlorite, zeolite, and quartz(?) veins in gabbro."	"isotropic gabbro rollers with localized occurences of protomylonite and fracturing"	
"399"	"U1601"	"C"	"193"	"R"	"2"	""	"399-U1601C-193R-2"	"0.0"	"123.0"	"950.880"	"951.495"	"952.110"	"950.88"	"951.495"	"952.11"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"The upper 59 cm is harzburgite with about 12% orthopyroxene and trace chromium spinel intermixed with gabbro with varying grain sizes. Below 59 cm is highly altered gabbro."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic vein composed of chlorite and amphibole. Highly altered gabbro. The mesh is black. Bastite is grey, black, and green. Mesh-forming serpentine-magnetite, chrysotile, picrolite, and magmatic veins in serpentinite. Talc-carbonate veins are present in gabbro."	"gabrro and harz rollers. protomylonitic interval in both lithologies. undeformed gabbro intruding against protomylonitic serp harz."	
"399"	"U1601"	"C"	"194"	"R"	"1"	""	"399-U1601C-194R-1"	"0.0"	"147.0"	"954.200"	"954.935"	"955.670"	"954.2"	"954.935"	"955.67"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"This section is mostly highly deformed gabbros, with orthopyroxene-bearing dunite in the intervals of 15-35 and 79-91 cm. Olivine gabbro is between 35 and 79 cm."	"Variably altered gabbroic rocks and highly serpentinized Opx-bearing dunite.  Isotropic fine-grained domains are highly altered compared to deformed domains, forming greenish patches. Disseminated sulfides in the groundmass of the gabbroic rocks. The origin (primary or secondary) of the sulfides is uncertain. The mesh is black and brown. Bastite is black and greenish grey. No spinel is visible. Serpentine-magnetite and chrysotile veins in serpentinite.Chlorite-amphibole, talc-carbonate, and zeolite veins in gabbroic rocks."	"protomylonitic gabbro in contact with serp harz, and protomylonitic gabbro foliation cut by microgabbro"	
"399"	"U1601"	"C"	"194"	"R"	"2"	""	"399-U1601C-194R-2"	"0.0"	"128.0"	"955.670"	"956.310"	"956.950"	"955.67"	"956.31"	"956.95"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"This section is medium-grained granular gabbro continuing from the overlying section. The interval between 0 and 11cm is strongly mylonitized. The interval between 62 and 67cm contains oxide-filled veins."	"Moderately altered Ol-bearing gabbroic rocks cut by chlorite, prehnite-amphibole-unidentified pink and grey minerals veins, and zeolite veins. Disseminated sulfides in the groundmass of the gabbroic rocks, possibly after olivine."	"partially protomylonitic gabbro crosscut by later shallow faults indicating reverse sense of shear"	
"399"	"U1601"	"C"	"195"	"R"	"1"	""	"399-U1601C-195R-1"	"0.0"	"150.0"	"959.100"	"959.850"	"960.600"	"959.1"	"959.85"	"960.6"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"This section is entirely medium-grained granular to subophitic gabbro with variation in grain size and texture down section. It is continuous from the overlying section."	"Slightly altered Ol-gabbro cut by a set of amphibole, talc-carbonate, and zeolite veins. Some disseminated sulfides are present in gabbro groundmass and are possibly of primary origin."	"isotropic gabbro with grain size variation and protomylonitic gabbrorubble at the bottom"	
"399"	"U1601"	"C"	"195"	"R"	"2"	""	"399-U1601C-195R-2"	"0.0"	"117.0"	"960.600"	"961.185"	"961.770"	"960.6"	"961.185"	"961.77"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Down to 71 cm, this section is coarse-grained granular to subophitic gabbro It is continuous from the overlying section. The lower 30 cm is harzburgite with 13% orthopyroxene and trace chromium spinel."	"Variably altered gabbroic rocks cut by amphibole, talc-carbonate-sulfide, and zeolite veins. The alteration extent increases at the bottom of the section, where the rock is fine-grained (chilled margin?) and appears greenish (possibly talc or clay minerals), and contains sulfides."	"gabbro showing increasing strain from protomylonite to mylonite downsection to serp harz contact. serp harz talcified, green-gre, but undeformed."	
"399"	"U1601"	"C"	"195"	"R"	"3"	""	"399-U1601C-195R-3"	"0.0"	"89.0"	"961.770"	"962.215"	"962.660"	"961.77"	"962.215"	"962.66"	""	"1, 2"	""	"This section is highly altered medium-grained gabbronorite. Both pyroxenes were confirmed by pXRF."	"Highly altered gabbroic rock cut by chlorite, talc-carbonate, and zeolite veins. Brown-stained after Cpx is present in the top of this section."	"very altered coarse grained gabbronorite cut by white green veins which are faulted. lots of rubble peices"	
"399"	"U1601"	"C"	"196"	"R"	"1"	""	"399-U1601C-196R-1"	"0.0"	"145.0"	"963.900"	"964.625"	"965.350"	"963.9"	"964.625"	"965.35"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is entirely medium-grained gabbro. It contains oxides between 81 and 90cm."	"Slightly to moderately altered Ol- and Ox-bearing gabbro cut by hydrothermally overprinted magmatic veins made of plagioclase and chlorite, amphibole veins, and chlorite vein. Disseminated sulfides are present in the groudmass, and locally associated with oxides."	"pyroxene rich gabbro / pyroxenite mostly isotropic undeformed with localised magmatic foliation and strong possible deformatoin folication"	
"399"	"U1601"	"C"	"196"	"R"	"2"	""	"399-U1601C-196R-2"	"0.0"	"125.0"	"965.350"	"965.975"	"966.600"	"965.35"	"965.975"	"966.6"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is entirely coarse-grained granular gabbro."	"Slightly to moderately coarse-grained altered gabbro cut by amphibole, chlorite, and zeolite veins. Localized small sulfides in amphibole after clinopyroxene and in clinopyroxene (primary origin possible)."	"isotropic coarse crained pyroxene rich gabbro / pyroxenite with protomylonite intervales"	
"399"	"U1601"	"C"	"197"	"R"	"1"	""	"399-U1601C-197R-1"	"0.0"	"79.0"	"968.800"	"969.195"	"969.590"	"968.8"	"969.195"	"969.59"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is coarse-grained granular gabbro like that in the overlying section. It contains domains of olivine-bearing gabbros and orthopyroxene-bearing dunite below 38 cm. "	"Moderately to highly altered gabbro, grain size is variable. Alteration is more extensive in fine-grained gabbro than in coarse-grained gabbro. One pebble of highly serpentinized Opx-bearing dunite at the end of the section. Mesh is brown-black. Bastite is black. Serpentine and serpentine-magnetite veins in the serpentinite. Gabbro is cut by amphibole, talc-carbonate, and zeolite veins."	"isotropic coarse crained pyroxene rich gabbro / pyroxenite with protomylonite intervals above green altered isotropic gabbro above gabbro mylonite above serp harz"	
"399"	"U1601"	"C"	"198"	"R"	"1"	""	"399-U1601C-198R-1"	"0.0"	"150.0"	"973.600"	"974.350"	"975.100"	"973.6"	"974.35"	"975.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21"	""	"The uppermost 21 cm is harzburgite with 10 % orthopyroxene and trace chromium spinel. A discrete vein of  gabbro cuts the harzburgite from 6-14 cm. Below is gabbro with oxides appearing at 38 cm and increasing in proportion down section. "	"Slightly to moderately altered oxide gabbro and highly serpentinized harzburgite cut by hydrothermally altered magmatic veins composed of Cpx, plagioclase, secondary plagioclase, chlorite, prehnite, and amphibole. The mesh is brown-black. Bastite is black and green. Sulfide is present in the gabbro matrix and associated with oxide and primary silicates. Serpentine and serpentine-magnetite veins, chrysotile, picrolite, and magmatic veins are present in the serpentinite. Gabbro is cut by amphibole, chlorite, and zeolite veins."	"weakly porphyroclastic serpentinized harzburgite, oxide gabbro, first isotropic, then moderately dipping foliated and protomylonitic, then isotropic"	
"399"	"U1601"	"C"	"198"	"R"	"2"	""	"399-U1601C-198R-2"	"0.0"	"106.0"	"975.100"	"975.630"	"976.160"	"975.1"	"975.63"	"976.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is coarse-grained granular oxide gabbro with oxide proportions continuing to inclrease down section. It is slightly deformed."	"Slightly to moderately altered oxide gabbro. Oxide is highly abundant. Sulfide is present in oxide-rich parts. Amphibole-chlorite vein set exists."	"isotropic gabbro, weakly protomylonitic oxide gabbro"	
"399"	"U1601"	"C"	"198"	"R"	"3"	""	"399-U1601C-198R-3"	"0.0"	"79.0"	"976.160"	"976.555"	"976.950"	"976.16"	"976.555"	"976.95"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is medium-grained, granular gabbro with seriate grain size distribution. It contains trace oxide."	"Slightly altered oxide-bearing gabbro. Oxide is highly abundant. Sulfide is present in oxide-rich parts. Talc + prehnite, and unidentified white veins."	"isotropic gabbro with grain size variation"	
"399"	"U1601"	"C"	"199"	"R"	"1"	""	"399-U1601C-199R-1"	"0.0"	"141.0"	"978.500"	"979.205"	"979.910"	"978.5"	"979.205"	"979.91"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Most of this section is medium-grained, granular gabbro with seriate grain size distribution. It contains trace oxide near the top. Coarse-grained granular gabbro domains are present as irregular, random patches at 54-60cm, 65-90cm, 99-105cm. Orthopyroxene-bearing dunite pebbles are present from 4-9 cm."	"Slightly altered oxide-bearing gabbro, and a piece of serpentinite rubble. A small amount of sulfide is associated with primary silicates in the gabbro. Talc rubble is present at the bottom of the section. The gabbro is cut by amphibole veins and talc (possibly clay-bearing) veins."	"isotropic gabbro with grain size variations and contacts"	
"399"	"U1601"	"C"	"199"	"R"	"2"	""	"399-U1601C-199R-2"	"0.0"	"145.0"	"979.910"	"980.635"	"981.360"	"979.91"	"980.635"	"981.36"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is medium-grained gabbro down to 67 cm, and is underlain by coarse-grained gabbro with zones of ophitic and subophitic textures."	"Slightly altered gabbro. Sulfide is associated with primary silicates. The degree of alteration increases in the vicinity of veins, where the clinopyroxene is replaced by chlorite/clay with a brown stain and plagioclase by chlorite and secondary plagioclase. The gabbro is cut by amphibole, and talc-prehnite veins."	"isotropic gabbro with slightly increasing grain size towards the bottom"	
"399"	"U1601"	"C"	"199"	"R"	"3"	""	"399-U1601C-199R-3"	"0.0"	"148.0"	"981.360"	"982.100"	"982.840"	"981.36"	"982.1"	"982.84"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is coarse-grained gabbro with zones of ophitic and subophitic textures. A fine-grained subophitic gabbro domain forms a patch at 38-42cm."	"Slightly altered oxide-bearing gabbro that is cut by amphibole veins and talc-carbonate veins."	"isotropic gabbro with grain size variations"	
"399"	"U1601"	"C"	"199"	"R"	"4"	""	"399-U1601C-199R-4"	"0.0"	"23.0"	"982.840"	"982.955"	"983.070"	"982.84"	"982.955"	"983.07"	""	"1, 2, 3, 4"	""	"This section is medium-grained granular olivine-bearing gabbro with seriate grain size distribution."	"Slightly altered olivine-bearing gabbro that is cut by amphibole-chlorite veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"200"	"R"	"1"	""	"399-U1601C-200R-1"	"0.0"	"135.0"	"983.300"	"983.985"	"984.670"	"983.3"	"983.985"	"984.67"	""	"1"	""	"This section is medium-grained largely granular olivine-bearing gabbro. A coarse-grained hornblende diorite domain is present at 9-37cm and 77-81cm."	"Moderately altered gabbro with abundant amphibole. The gabbro is cut by amphibole veins with a thick halo and talc-carbonate veins."	"isotropic gabbro with grain size varation and compositional variations"	
"399"	"U1601"	"C"	"200"	"R"	"2"	""	"399-U1601C-200R-2"	"0.0"	"135.0"	"984.670"	"985.345"	"986.020"	"983.99"	"984.33"	"984.67"	""	"1"	""	"This section continues the medium-grained olivine-bearing gabbro. "	"Moderately altered gabbro with abundant amphibole in a vein halo. The gabbro is cut by amphibole veins with a thick halo and talc-carbonate veins."	"isotropic gabbro with increasing grain size towards the bottom"	
"399"	"U1601"	"C"	"200"	"R"	"3"	""	"399-U1601C-200R-3"	"0.0"	"52.0"	"986.020"	"986.300"	"986.580"	"985.556"	"985.788"	"986.02"	""	"1"	""	"This section continues the medium-grained olivine-bearing gabbro. "	"Slightly altered gabbro. Alteration degree increases toward veins. The gabbro is cut by amphibole veins and zeolite veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"201"	"R"	"1"	""	"399-U1601C-201R-1"	"0.0"	"149.0"	"988.200"	"988.945"	"989.690"	"988.2"	"988.945"	"989.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Medium- to coarse-grained gabbronorite with rare veins of medium-grained granular diorite. "	"Slightly altered gabbro. Alteration degree increases towards veins (amphibole and talc-carbonate veins). Close to talc-carbonate veins, clinopyroxene is replaced by a clay/chlorite mixture (light brown stain). Prehnite forms after plagioclase. Close to amphibole veins, clinopyroxene is replaced by amphibole and secondary plagioclase forms after plagioclase."	"isotropic gabbro with increasing grain size towards the bottom"	
"399"	"U1601"	"C"	"201"	"R"	"2"	""	"399-U1601C-201R-2"	"0.0"	"112.0"	"989.690"	"990.250"	"990.810"	"989.69"	"990.25"	"990.81"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Medium-grained and granular gabbronorite. "	"Slightly altered Ol-bearing gabbro. Alteration degree increases towards veins. Close to talc-carbonate veins clinopyroxene is replaced by clays/chlorite mixture (light brown stain) and prehnite forms after plagioclase. Close to amphibole veins clinopyroxene is replaced by amphibole and secondary plagioclase plus chlorite form after plagioclase. Close to zeolite veins, olivine is altered to clays and sulfides occur in the groundmass."	"Isotropic gabbro crosscut by various green and black veins with shallow to moderate dips."	
"399"	"U1601"	"C"	"201"	"R"	"3"	""	"399-U1601C-201R-3"	"0.0"	"140.0"	"991.120"	"991.820"	"992.520"	"991.12"	"991.82"	"992.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Gabbronorite with grain sizes varying from fine to coarse. Sulfides are present near the base of the section. "	"Slightly altered olivine- and oxide-bearing gabbro. Olivine-rich interval occurs at 77-85 cm. The alteration degree increases toward veins. Primary sulfides (pyrrhotite, chalcopyrite, bornite) are associated with primary silicates, and secondary sulfides also exist. The abundance of primary sulfides is variable throughout the section. The degree of clinopyroxene, olivine, and plagioclase alteration is high near talc-carbonate veins. Talc-carbonate and zeolite veins."	"isotropic gabbro with grain size contacts, gabbro with moderately dipping magmatic fabric parallel to contact"	
"399"	"U1601"	"C"	"201"	"R"	"4"	""	"399-U1601C-201R-4"	"0.0"	"46.0"	"992.520"	"992.750"	"992.980"	"992.52"	"992.75"	"992.98"	""	"1, 2, 3, 4"	""	"Granular gabbronorite with widely ranging grain sizes (fine to coarse). Trace oxides are present near the base of the section."	"Slightly altered olivine- and oxide-bearing gabbro. Sulfides are associated with amphibole after clinopyroxene. Locally higher degrees of alteration occurs near veins."	"Gabbro with intervals of isotropic and SPO (magmatic fabric; 30deg).  Grain size contact (30deg).  Cut by green-black (0deg) and black-white veins (40deg)."	
"399"	"U1601"	"C"	"202"	"R"	"1"	""	"399-U1601C-202R-1"	"0.0"	"149.0"	"993.000"	"993.745"	"994.490"	"993"	"993.745"	"994.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Coarse-grained granular gabbronorite."	"Slightly altered Ol-bearing gabbro. Talc-carbonate and zeolite veins."	"isotropic gabbro, gabbro with moderately inclined SPO formed by pyroxene, isotropic gabbro"	
"399"	"U1601"	"C"	"202"	"R"	"2"	""	"399-U1601C-202R-2"	"0.0"	"149.0"	"994.490"	"995.235"	"995.980"	"994.49"	"995.235"	"995.98"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Mostly coarse-grained granular gabbronorite. The basal 29 cm is medium-grained."	"Slightly altered Ol-bearing gabbro. Degree of alteration increases near talc-carbonate veins. Disseminated primary sulfide exists throughout the section. Talc-carbonate and zeolite veins."	"isotropic gabbro and gabbro with SPO"	
"399"	"U1601"	"C"	"202"	"R"	"3"	""	"399-U1601C-202R-3"	"0.0"	"144.0"	"995.980"	"996.700"	"997.420"	"995.98"	"996.7"	"997.42"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Medium to coarse-grained granular gabbronorite"	"Slightly altered coarse-grained gabbro. Degree of alteration increases near quartz veins. Talc-carbonate, quartz, and zeolite veins."	"isotropic gabbro, grain size variation"	
"399"	"U1601"	"C"	"202"	"R"	"4"	""	"399-U1601C-202R-4"	"0.0"	"25.0"	"997.420"	"997.545"	"997.670"	"997.42"	"997.545"	"997.67"	""	"1, 2"	""	"Coarse-grained granular granular gabbronorite. "	"Slightly altered coarse-grained gabbro that is cut by zeolite veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"203"	"R"	"1"	""	"399-U1601C-203R-1"	"0.0"	"136.0"	"997.900"	"998.580"	"999.260"	"997.9"	"998.58"	"999.26"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Fine to coarse grained gabbro and olivine-bearing gabbro."	"Slightly altered gabbro to olivine-bearing gabbro with variable grain size. Degree of alteration increases near hydrothermal veins. A small amount of disseminated primary sulfide exists throughout the section. Talc-carbonate and zeolite veins."	"isotropic gabbro with decreasing grain size towards 110cm, then grain size contact with coarser gabbro"	
"399"	"U1601"	"C"	"203"	"R"	"2"	""	"399-U1601C-203R-2"	"0.0"	"138.0"	"999.260"	"999.950"	"1000.640"	"999.26"	"999.95"	"1000.64"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is fine- to coarse-grained, subophitic olivine bearing gabbro down to 44 cm. Coarse-grained orthopyroxene bearing gabbro is below"	"Slightly altered olivine-bearing gabbro. A small amount of disseminated primary sulfide exists throughout the section. Secondary plagioclase and prehnite appear close to amphibole veins and talc-carbonate veins, respectively. Zeolite veins are also present in this section."	"isotropic gabbro with moderately dipping grain size layering, weak magmatic SPO fabric at the bottom"	
"399"	"U1601"	"C"	"203"	"R"	"3"	""	"399-U1601C-203R-3"	"0.0"	"143.0"	"1000.640"	"1001.355"	"1002.070"	"1000.64"	"1001.355"	"1002.07"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is orthopyroxene-bearing gabbro with variable grain size down to 90 cm. Below is a coarse-grained disseminated oxide gabbronorite."	"Slightly altered olivine-bearing gabbro. A small amount of disseminated primary sulfide exists throughout the section. Talc-carbonate, quartz and zeolite veins."	"isotropic gabbro with grain size variations and weak magmatic SPO at the bottom"	
"399"	"U1601"	"C"	"204"	"R"	"1"	""	"399-U1601C-204R-1"	"0.0"	"146.0"	"1002.700"	"1003.430"	"1004.160"	"1002.7"	"1003.43"	"1004.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The disseminated oxide gabbronorite from the overlying section continues down to 80cm. It is underlain by medium-grained gabbronorite."	"Moderately altered olivine-bearing gabbro with oxide-gabbro at the top of the section. Degree of alteration increases toward hydrothermal veins. Close to amphibole veins, amphibole and secondary plagioclase are conspicuous. Close to talc-carbonate veins, clay/chlorite after Cpx exists. Three types of veins are amphibole +/- sulfide +/- oxide, talc + carbonate, and zeolite."	"isotropic gabbro, weakly magmatically folaited gabbro, grain size boundary to isotropic fine grained gabbro"	
"399"	"U1601"	"C"	"204"	"R"	"2"	""	"399-U1601C-204R-2"	"0.0"	"139.0"	"1004.160"	"1004.855"	"1005.550"	"1004.16"	"1004.855"	"1005.55"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is coarse-grained orthopyroxene-bearing gabbro down to 51 cm. Domains of dunite (65%) and gabbronorite (35%) are below."	"Variably altered olivine-bearing gabbro and highly serpentinized dunite cut by hydrothermally altered magmatic veins composed of chlorite, brown-stained Cpx, and secondary plagioclase. Degree of alteration of gabbro (with greenish to whitish color) increases toward serpentinite contact. Fracture surfaces of serpentinized dunite (35-53cm) are coated with sulfide (likely pyrrhotite). Mesh is brown and black. Bastite is brown. Serpentine and serpentine-magnetite veins in serpentinite. Talc-carbonate, quartz, and zeolite veins in gabbro."	"isotropic gabbro, weakly foliated serp dunite with chalcopyrite in faults showing slicks, isotropic gabbro"	
"399"	"U1601"	"C"	"205"	"R"	"1"	""	"399-U1601C-205R-1"	"0.0"	"150.0"	"1007.600"	"1008.350"	"1009.100"	"1007.6"	"1008.35"	"1009.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Gabbronorite with minor intervals or domains of olivine-bearing gabbro, orthopyroxene-bearing dunite, and dunite."	"Variably altered gabbro and minor moderately serpentinized harzburgite. Near contact between gabbro and serpentinized harzburgite, gabbro is green and rich in amphibole. Olivine in harzburgite close to the contact with gabbro is associated with sulfide and shows a brown stain. Amphibole, talc + carbonate + prenite +/- sulfide, and zeolite veins in gabbro. Serpentine and serpentine-magnetite veins in serpentinite."	"fractured gabbro with grain size and alteration variations, contact to harzburgite at bottom"	
"399"	"U1601"	"C"	"205"	"R"	"2"	""	"399-U1601C-205R-2"	"0.0"	"119.5"	"1009.100"	"1009.697"	"1010.295"	"1009.1"	"1009.697"	"1010.295"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"The top of this section is harzburgite infused with gabbroic material. Below 91 cm is entirely medium-grained, granular to subophitic gabbro."	"Moderately altered gabbro to troctolite and moderately serpentinized harzburgite and highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins composed of Cpx, plagioclase, secondary plagioclase, and chlorite. The abundance of relict olivine is variable. Mesh is black to grey and in harzburgite, appears golden brown (rich in sulfide?) near the contact with the gabbroic rock. Bastite is black. Serpentine and serpentine-magnetite and serpentine-sulfide mesh-forming veins, picrolite, and magmatic veins in serpentinite. Amphibole, talc + carbonate + sulfide, and zeolite veins in gabbro."	"harzburgite and gabbro, gabbroprotomylonite with steep foliatio at bottom"	
"399"	"U1601"	"C"	"206"	"R"	"1"	""	"399-U1601C-206R-1"	"0.0"	"150.0"	"1012.400"	"1013.150"	"1013.900"	"1012.4"	"1013.15"	"1013.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly coarse-grained granular gabbronorite with trace oxide. Patches of medium-grained gabbro make up 10% of the section"	"Variably altered gabbro, oxide-bearing gabbro, and Ol-bearing gabbro. The degree of alteration increases toward hydrothermal veins. Sulfide is rich in oxide-gabbro and is disseminated throughout the section. Amphibole, talc, and zeolite veins."	"isotropic coarse grained gabbro with a mylonite at an intrusive contact? at 23 cm"	
"399"	"U1601"	"C"	"206"	"R"	"2"	""	"399-U1601C-206R-2"	"0.0"	"122.5"	"1013.900"	"1014.513"	"1015.125"	"1013.9"	"1014.513"	"1015.125"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Gabbronorite with grain size varying from medium to coarse grained and unevenly distributed. Slightly deformed. Cpx grain size up to 38mm. Trace oxide is present."	"Slightly altered gabbro and  oxide (primary or secondary) -bearing gabbro. The degree of alteration tends to increase toward hydrothermal veins. Sulfide is rich in oxide-gabbro and is disseminated throughout the section. Amphibole, quartz, and zeolite veins."	"isotropic coarse grained gabbro, with protomylonite in rubble pieces"	
"399"	"U1601"	"C"	"206"	"R"	"3"	""	"399-U1601C-206R-3"	"0.0"	"63.0"	"1015.200"	"1015.515"	"1015.830"	"1015.2"	"1015.515"	"1015.83"	""	"1, 2, 3, 4"	""	"This section is coarse grained granular gabbronorite. Trace oxide is concentrated at 10 cm."	"Slightly altered coarse-grained gabbro and minor oxide-bearing gabbro. Sulfide is disseminated throughout the section. Amphibole, quartz, and zeolite veins."	"coarse grained isotropic gabbro"	
"399"	"U1601"	"C"	"207"	"R"	"1"	""	"399-U1601C-207R-1"	"0.0"	"139.0"	"1017.300"	"1017.995"	"1018.690"	"1017.3"	"1017.995"	"1018.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Coarse-grained, granular gabbronorite  continued from the previous section. The gabbronorite has disseminated oxides (1%) in the middle of the section. Cpx grains as large as 35mm. "	"Variably altered gabbro (rubble). The extent of alteration is locally high (35-45 cm). Talc + carbonate and zeolite veins."	"coarse grained isotropic gabbro with a cataclastic zone at 36-45 cm"	
"399"	"U1601"	"C"	"208"	"R"	"1"	""	"399-U1601C-208R-1"	"0.0"	"104.0"	"1022.100"	"1022.620"	"1023.140"	"1022.1"	"1022.62"	"1023.14"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Coarse-grained, seriate granular gabbronorite."	"Variably altered gabbro and olivine gabbro (top of the section). The extent of alteration increases near veins. Sulfide is associated with olivine. Clay/chlorite after Cpx and prehnite after plagioclase exist near veins. Amphibole, talc + carbonate, and zeolite veins."	"isotropic gabbro with rollers of protomylonitic gabbro, magmatic breccia at 35-47"	
"399"	"U1601"	"C"	"209"	"R"	"1"	""	"399-U1601C-209R-1"	"0.0"	"149.0"	"1027.000"	"1027.745"	"1028.490"	"1027"	"1027.745"	"1028.49"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"The coarse-grained, granular gabbro with trace oxide.  Orthopyroxene-bearing dunite with trace chromium spinel is below 116 cm."	"Slightly altered gabbro and highly serpentinized Opx-bearing dunite. Mesh is black-brown. Bastite is black, grey, and locally green. Spinel is fresh. Serpentinite features serpentine-magnetite veins in mesh texture. Gabbro features amphibole, prehnite, talc, and zeolite veins."	"isotropic oxide gabbro, a different, melt infiltrated and slightly deformed gabbro towards contact with protogranular serpentinized harzburgite"	
"399"	"U1601"	"C"	"209"	"R"	"2"	""	"399-U1601C-209R-2"	"0.0"	"126.0"	"1028.490"	"1029.120"	"1029.750"	"1028.49"	"1029.12"	"1029.75"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The orthopyroxene-bearing dunite with trace chromium spinel continues from the previous section down to 103 cm. The rest of the section is coarse-grained gabbro ."	"Highly serpentinized Opx-bearing dunite and slightly altered gabbro. The mesh is black to brown. Bastite is black and grey. Spinel is fresh. Serpentinite features serpentine-magnetite veins in mesh texture, chrysotile veins, and a brown vein featuring an unidentified mineral. Gabbro features zeolite veins."	"weakly porphyroclastic serpentinized harzburgite, isotropic gabbro"	
"399"	"U1601"	"C"	"209"	"R"	"3"	""	"399-U1601C-209R-3"	"0.0"	"62.0"	"1029.750"	"1030.060"	"1030.370"	"1029.75"	"1030.06"	"1030.37"	""	"1, 2, 3, 4, 5, 6"	""	"The coarse-grained, granular gabbro continues from the previous section down to 52 cm. The rest of the section is orthopyroxene-bearing dunite."	"Moderately gabbro and Ol-gabbro, as well as highly serpentinized Opx-bearing dunite. Mesh is black-brown. Bastite is grey and black. Spinel is fresh. Fracture surfaces of Opx-bearing dunite are coated in sulfide. Serpentinite is cut by serpentine-magnetite and sulfide-carbonate veins. Gabbro is cut by amphibole and zeolite veins."	"weakly protomylonitic gabbro, serpentinized harzburgite"	
"399"	"U1601"	"C"	"210"	"R"	"1"	""	"399-U1601C-210R-1"	"0.0"	"131.0"	"1031.800"	"1032.455"	"1033.110"	"1031.8"	"1032.455"	"1033.11"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The top and bottom of this section is orthopyroxene-bearing dunite. From 7 to 121cm, the section is coarse-grained, granular gabbro like that in the previous section."	"Variably altered gabbroic rock and pieces of highly serpentinized Opx-bearing dunite at the top and bottom (below 120 cm) of the section. The gabbro is cut by talc, amphibole, and zeolite veins, and prehnite and a brown unidentified mineral are present close to the contact with the serpentinite. In the serpentinite, the mesh is black, brown, and grey, bastites are black and grey, and spinel is mostly fresh. The serpentine mesh texture is cut by subparallel fibrous to massiv chrysotile veins. "	"protomylonitic gabbro, less deformed towards the contact with serpentinized harzbrugtie, no veins"	
"399"	"U1601"	"C"	"210"	"R"	"2"	""	"399-U1601C-210R-2"	"0.0"	"85.0"	"1033.110"	"1033.535"	"1033.960"	"1033.11"	"1033.535"	"1033.96"	""	"1, 2"	""	"This section is mostly harzburgite with trace spinel and c. 5% diffuse gabbro veins."	"Highly serpentinized Opx-bearing dunite with hydrothermally altered magmatic veins composed of clinopyroxene, plagioclase, chlorite, and secondary plagioclase. The clinopyroxene locally shows a brown stain. The mesh is brown black and locally greenish grey, the bastites are black, grey, and green, and spinel is mostly fresh. The serpentine mesh texture is cut by a dense network of subparallel fibrous chrysotile veins, and locally picrolite veins that also cut the hydrothermally altered magmatic veins."	"protogranular serpentinized harzburgite, then weakly porphyroclastic serpentinized harzburgite with horizontal foliation"	
"399"	"U1601"	"C"	"210"	"R"	"3"	""	"399-U1601C-210R-3"	"0.0"	"131.0"	"1033.960"	"1034.615"	"1035.270"	"1033.96"	"1034.615"	"1035.27"	""	"1, 2, 3, 4"	""	"This section is all peridotite, varying from dunite with no orthopyroxene to harzburgite with c. 30 % orthopyroxene. The dunite at 54 to 66 cm has a trail of relatively coarse grained chromium spinel. Plagioclase may impregnate the peridotites in the bottom half of the section."	"Highly serpentinized harzburgite and dunite with abundant fresh spinel that occurs in dunite at the contact with harzburgite. The mesh is grey and brown, and locally greenish grey (abundant in dunite) and the bastites are black and green. The serpentine mesh texture is cut by serpentine-magnetite and chrysotile veins that are locally associted with carbonate, as well as a vein composed of a brown unidentified mineral."	"serpentinized harzburgite with weak porphyroclastic foliation dipping shallow and dunite with weak mesh dipping shallow in the same orientation"	
"399"	"U1601"	"C"	"210"	"R"	"4"	""	"399-U1601C-210R-4"	"0.0"	"132.0"	"1035.270"	"1035.930"	"1036.590"	"1035.27"	"1035.93"	"1036.59"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is mostly peridotite, varying from dunite with 4-5 % orthopyroxene to harzburgite with c. 15 % orthopyroxene. Trace chromium spinel is throughout. A pervasively altered gabbro cuts the section at c. 93 cm. The section terminates in 23 cm of coarse-grained granular gabbro."	"Highly serpentinized harzburgite and dunite cut by hydrothermally altered magmatic vein composed of brown-stained clinopyroxene, secondary plagioclase, and chlorite. The section also contains moderately altered gabbro toward the bottom of the section. The mesh is grey, black, and locally greenish grey and the bastites are black, grey, and locally green. The serpentine mesh texture is cut by sets of subparallel fibrous chrysotile veins that vary in abundance, and picrolite veins that also cut the hydrothermally altered magmatic veins."	"Protogranular to moderately porphyroclastic mantle fabric (20 and 30deg) and weakly foliated serpentine foliation (moderate-shallow dip) in serp harz. Dunite has a moderate serpentine foliation (35deg). Crosscut by several veins including magmatic (15deg), white (20-40deg) and a subhorizontal red vein.  Two of the white veins are faults with slickenlines that have shallow plunges."	
"399"	"U1601"	"C"	"211"	"R"	"1"	""	"399-U1601C-211R-1"	"0.0"	"150.0"	"1036.700"	"1037.450"	"1038.200"	"1036.7"	"1037.45"	"1038.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"This section is coarse-grained oxide-bearing gabbro with varying proportions of oxides. "	"Slightly to moderately altered and variably deformed oxide gabbro to oxide-bearing gabbro that are cut by amphibole and chlorite veins. Sulfides are preferentially associated with oxides. "	"undeformed and protomylonitic to mylonitic gabbro, moderately dipping, some of it oxide-bearing"	
"399"	"U1601"	"C"	"211"	"R"	"2"	""	"399-U1601C-211R-2"	"0.0"	"146.0"	"1038.200"	"1038.930"	"1039.660"	"1038.2"	"1038.93"	"1039.66"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Coarse- to medium-grained gabbro with a variable proportion of oxide (trace to 10%). From 37 to 50 cm is a coarse-grained granular troctolite with cpx proportion increasing down section. "	"Slightly to moderately altered and variably deformed oxide-bearing to oxide gabbro and troctolite. Sulfides are disseminated throughout the section. The extent of hydrothermal alteration increases close to the talc-carbonate veins. There, prehnite and clay-chlorite form after plagioclase and clinopyroxene, respectively. Amphibole, talc-carbonate, and zeolite veins occur in the gabbro."	"protomylonitc to mylonitic gabbro, shallow to moderately dipping, with a piece of troctolite or harzburgite as rubble included"	
"399"	"U1601"	"C"	"211"	"R"	"3"	""	"399-U1601C-211R-3"	"0.0"	"21.0"	"1039.660"	"1039.765"	"1039.870"	"1039.66"	"1039.765"	"1039.87"	""	"1, 2"	""	"Medium-grained granular gabbro with trace oxide."	"Moderately altered and variably deformed gabbro that is cut by zeolite veins. Magmatic sulfides occur disseminated in the gabbro throughout the section."	"Isotropic to strongly foliated gabbro (45deg)."	
"399"	"U1601"	"C"	"212"	"R"	"1"	""	"399-U1601C-212R-1"	"0.0"	"150.0"	"1041.500"	"1042.250"	"1043.000"	"1041.5"	"1042.25"	"1043"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The first 47 cm of this section is gabbro that varies from coarse to medium grained. Harzburgite with10% orthopyroxene, trace chromium spinel is below to the base of the section. The harzburgite is cut by a few veins of pervasively altered gabbro."	"Slightly to moderately altered gabbro at the top of the section and highly serpentinized harzburgite below 47 cm. The gabbro is cut by amphibole and zeolite veins. The serpentinized harzburgite is cut by hydrothermally altered magmatic veins composed of serpentine(?), chlorite, and amphibole to plagioclase, secondary plagioclase, clinopyroxene, amphibole, and sulfides. In the serpentinite, the mesh is brown-black to locally black-grey. Close to the magmatic veins, some mesh cores are associated with yellow sulfides. The bastites form a black corona around fresh orthopyroxene. The serpentine mesh texture is cut by subparallel fibrous to massive chrysotile veins, and picrolite veins cut the hydrothermally altered magmatic veins."	"undeformed isotropic gabbro with grain size contacts, weakly prophyroclastic to protogranular serpentinized harzburgite"	
"399"	"U1601"	"C"	"212"	"R"	"2"	""	"399-U1601C-212R-2"	"0.0"	"149.5"	"1043.005"	"1043.753"	"1044.500"	"1043.005"	"1043.753"	"1044.5"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Harzburgite with trace spinel down to 47 cm. Below to the bottom of the section is coarse-grained granular gabbro with pegmatitic crystals perpendicular to the upper contact. "	"Highly serpentinized harzburgite at the top of the section and slightly to moderately altered gabbro below 46 cm. The serpentinized harzburgite is cut by hydrothermally altered magmatic veins composed of chlorite and amphibole. The mesh is greenish-grey to brown-black, the bastites are black, and spinel is fresh. The serpentine mesh texture is cut by subparallel fibrous chrysotile veins and picrolite veins cut the hydrothermally altered magmatic veins. The gabbro is cut by amphibole, talc, and zeolite veins and the extent of alteration in the gabbro increases toward the contact with the serpentinite."	"weakly porphyroclastic harzburgite with shallow dip in moderate contact with gabbro, which is protomylonitic, the contact is crosscut and offset by faults +1cm , veins occur only close to the contact"	
"399"	"U1601"	"C"	"212"	"R"	"3"	""	"399-U1601C-212R-3"	"0.0"	"79.0"	"1044.500"	"1044.895"	"1045.290"	"1044.5"	"1044.895"	"1045.29"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Coarse-grained granular gabbro with pegmatitic grains perpendicular to the boundary down to 15 cm. The rest of the section is  coarse-grained gabbro, with an interval of dunite at 15-22 cm. Oxide gabbro with trace sulfide makes up the interval between 59 and 67 cm."	"Moderately to highly altered gabbro and slightly altered oxide gabbro. There are two pebbles of highly serpentinized Opx-bearing dunite near the top of the section. The gabbro is cut by amphibole, talc, and zeolite veins and locally sulfides are associated with the oxide gabbro."	"protomylonitic gabbro, followed by fractured and veined coarse grained gabbro, followed by undeformed coarse and fine grained gabbro"	
"399"	"U1601"	"C"	"213"	"R"	"1"	""	"399-U1601C-213R-1"	"0.0"	"146.0"	"1046.400"	"1047.130"	"1047.860"	"1046.4"	"1047.13"	"1047.86"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"The upper 75 cm is orthopyroxene-bearing dunite with trace spinel. Its orthopyroxene content decreases down section toward the underlying gabbro. A gabbronorite vein cuts steeply through this interval. From 75 to 104 cm is a coarse-grained, granular gabbro with significant grain size variation. Harzburgite with 20% orthopyroxene and trace chromium spinel and clinopyroxene is below 104 cm."	"Highly and variably serpentinized harzburgite with an interval of highly altered gabbro in the middle of the section. The serpentinized harzburgite is cut by hydrothermally altered magmatic veins composed of secondary plagioclase, chlorite, and brown-stained clinopyroxene. The harzburgite is less serpentinized between 120 and 150 cm. The mesh is brown-black, the bastites are black and green, and spinel is fresh. The serpentinite is cut by rare fibrous chrysotile veins and green massive picrolite veins cut the hydrothermally altered magmatic veins. The gabbro is cut by amphibole and talc veins."	"protogranular serpentinized harzburgite, contact with gabbro, magmatic breccia, serpentinized harzburgite with a strong porphyroclastic fabric dipping shallow"	
"399"	"U1601"	"C"	"213"	"R"	"2"	""	"399-U1601C-213R-2"	"0.0"	"146.0"	"1047.860"	"1048.590"	"1049.320"	"1047.86"	"1048.59"	"1049.32"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly harzburgite with 10% orthopyroxene and trace chromium spinel and clinopyroxene. This section is cut in several places by mm-scale gabbro veins."	"Highly serpentinized harzburgite and Opx-bearing dunite. Both are cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, secondary plagioclase, chlorite, and amphibole. The extent of serpentinization increases down section. The mesh is brown-black, the bastites are black and locally green along magmatic veins, and spinel is fresh. The serpentine mesh texture is cut by massive to fibrous chrysotile veins, and picrolite veins cut the hydrothermally altered magmatic vein."	"serpentinized harzburgite with strong porphyroclastic or protogranular mantle fabric and weakly foliated or regular mesh"	
"399"	"U1601"	"C"	"213"	"R"	"3"	""	"399-U1601C-213R-3"	"0.0"	"21.0"	"1049.320"	"1049.425"	"1049.530"	"1049.32"	"1049.425"	"1049.53"	""	"1, 2, 3"	""	"This section is mostly harzburgite with 10% orthopyroxene and trace chromium spinel and clinopyroxene. This section is cut a mm-scale gabbro vein."	"Highly serpentinized harzburgite and Opx-bearing dunite, that are cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, secondary plagioclase, chlorite, and amphibole. The mesh is brown-black, bastites are black and locally green along magmatic veins, and spinel is fresh."	"Protogranular serp harz with weakly foliated serpentine foliation (30deg) crosscut by a magmatic vein (90deg)."	
"399"	"U1601"	"C"	"214"	"R"	"1"	""	"399-U1601C-214R-1"	"0.0"	"149.0"	"1051.200"	"1051.945"	"1052.690"	"1051.2"	"1051.945"	"1052.69"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23"	""	"The uppermost 38 cm is orthopyroxene-bearing dunite cut by a 3-mm-wide highly altered gabbro vein. The rest of the section is coarse- to fine-grained granular gabbro. "	"Variably altered gabbro and slightly altered Ol-bearing gabbro (1 piece), and highly serpentinized Opx-bearing dunite (0-22 cm) cut by hydrothermally altered magmatic veins composed of secondary plagioclase, brown-stained clinopyroxene, chlorite, and amphibole. The gabbro is cut by amphibole, talc, and zeolite veins. The gabbro is more altered at the contact with the serpentinite, and the extent of alteration decreases down section. In the serpentinite, the mesh is brown-black, bastites are black, and spinel is not observed. The serpentine mesh texture is cut by fibrous chrysotile veins and picrolite veins that also cut the altered magmatic veins."	"protogranular harzburgite, coarse grained gabbro, partially protomylonitic with grain size variations"	
"399"	"U1601"	"C"	"214"	"R"	"2"	""	"399-U1601C-214R-2"	"0.0"	"142.0"	"1052.690"	"1053.400"	"1054.110"	"1052.69"	"1053.4"	"1054.11"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is mostly medium to coarse-grained granular to subophitic gabbro. The interval between 52 and 89 cm is predominantly orthopyroxene-bearing dunite with trace spinel."	"Slightly altered gabbro and highly serpentinized Opx-bearing dunite (16-47 cm) that is cut by hydrothermally altered magmatic veins composed of secondary plagioclase, brown-stained clinopyroxene, chlorite, and amphibole. Amphibole, talc, and zeolite veins are present in gabbro. In the serpentinite, the mesh is brown-black, and some sulfides are present in the mesh, locally close to the magmatic vein. The bastites are mostly black. The serpentine mesh texture is cut by fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	"protomylonitic gabbro, harzburgite with strong porphyroclastic fabric dipping 35 degrees, isotropic undeformed gabbro"	
"399"	"U1601"	"C"	"214"	"R"	"3"	""	"399-U1601C-214R-3"	"0.0"	"122.0"	"1054.115"	"1054.725"	"1055.335"	"1054.115"	"1054.725"	"1055.335"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is medium- to coarse-grained, granular to subophitic gabbro with a clear seriate grain size distribution."	"Slightly to moderately altered Ol-bearing gabbro that is cut by amphibole, zeolite, talc, and talc-zeolite veins that contain amphibole clasts of the gabbro host. Olivine is potentially altered to clays assocated with sulfide, preferentially close to the talc veins."	"isotropic gabbro with grain size variation and green veins"	
"399"	"U1601"	"C"	"215"	"R"	"1"	""	"399-U1601C-215R-1"	"0.0"	"148.0"	"1056.100"	"1056.840"	"1057.580"	"1056.1"	"1056.84"	"1057.58"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Most of this section is olivine-bearing gabbro with variable modes and grain sizes, although most is medium grained and subophitic. A section of fine grained subophitic gabbro is beneath 139 cm. "	"Moderately altered Ol-bearing gabbro. Olivine altered to clays (?) and sulfide, preferentially close to the talc veins. The first piece of the section is highly altered. Amphibole, chlorite, talc, talc-zeolite, and zeolite veins are present in the gabbro."	"mostly isotropic gabbro, a zone of weak protomylonite, and zone of magmatic SPO"	
"399"	"U1601"	"C"	"215"	"R"	"2"	""	"399-U1601C-215R-2"	"0.0"	"150.0"	"1057.580"	"1058.330"	"1059.080"	"1057.58"	"1058.33"	"1059.08"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"This section is entirely gabbro, with grain sizes varying from gine to coarse. Below 128 cm, textures are subophitic to ophitic with oikocrysts up to 48 mm across."	"Sightly altered gabbro and Ol-bearing gabbro. Olivine is altered to clay (?) minerals associated with sulfide, clinopyroxene altered to clay/chlorite, preferentially close to the talc veins. Amphibole, talc, and zeolite veins occur in the gabbro."	"gabbro with grain size variations"	
"399"	"U1601"	"C"	"215"	"R"	"3"	""	"399-U1601C-215R-3"	"0.0"	"144.0"	"1059.080"	"1059.800"	"1060.520"	"1059.08"	"1059.8"	"1060.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Fine-grained granular gabbro down to 19 cm, with medium-grained granular gabbro then subophic coarse-grained gabbro below. "	"Sightly to moderately altered Ol-bearing gabbro. The extent of alteration appears higher close to veins. Locally olivine is altered to clays (?) and sulfide. Clinopyroxene is altered to clay/chlorite. Amphibole, talc, and zeolite veins occur in the gabbro."	"isotropic gabbro with grain size variation"	
"399"	"U1601"	"C"	"215"	"R"	"4"	""	"399-U1601C-215R-4"	"0.0"	"17.0"	"1060.520"	"1060.605"	"1060.690"	"1060.52"	"1060.605"	"1060.69"	""	"1, 2, 3"	""	"Subophic coarse-grained gabbro. "	"Sightly to moderately altered gabbro that is cut by chlorite, amphibole, and zeolite veins. The extent of alteration appears higher close to the veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"216"	"R"	"1"	""	"399-U1601C-216R-1"	"0.0"	"141.0"	"1060.900"	"1061.605"	"1062.310"	"1060.9"	"1061.605"	"1062.31"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is dunite grading downward at c. 33 cm to harzburgite with 12% orthopyroxene with trace chromium spinel and clinopyroxene. The dunite is cut by a vein and patch of medium-grained olivine gabbro. Olivine near the contact is likely derived from host peridotite. Serpentine mesh texture extends from the serpentinite into the vein."	"Highly serpentinized harzburgite and dunite; the former is cut by hydrothermally altered magmatic veins composed of amphibole, chlorite, prehnite, and secondary plagioclase. A rubble of highly altered troctolite (0-7 cm) occurs at the contact with the serpentinized dunite. The overall extent of serpentinization is variable, becoming lower down section. Harzburgite is also less serpentinized close to the gabbro at the top of the section. The mesh is brown-black and bastites are green and black. Spinel is fresh. The serpentine mesh texture is cut by a large number of fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	"protogranular serpentinized harzburgite with shallowly inclined weakly foliated or regular mesh "	
"399"	"U1601"	"C"	"216"	"R"	"2"	""	"399-U1601C-216R-2"	"0.0"	"125.0"	"1062.310"	"1062.935"	"1063.560"	"1062.31"	"1062.935"	"1063.56"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is harzburgite with orthopyroxene proportions avaraging 13 %, but decreasing downsection. Contains both granular and intersitital orthopyroxene, and trace chlinopyroxene and Cr-spinel. Gabbronorite veins, 1-8 mm thick, cut through much of the length of the section."	"Highly serpentinized harzburgite and Opx-bearing dunite, both are cut by hydrothermally altered magmatic veins composed of secondary plagioclase, amphibole, chlorite, brown-stained clinopyroxene, and a pink mineral. The mesh is brown-black and the bastites are black and green. The serpentine mesh texture is cut by subparallel fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	"weakly porphyroclastic to ptorgranular serpentinized harzburgite with shallow dipping weakly folaited or regular mesh"	
"399"	"U1601"	"C"	"216"	"R"	"3"	""	"399-U1601C-216R-3"	"17.0"	"111.0"	"1063.730"	"1064.200"	"1064.670"	"1063.73"	"1064.2"	"1064.67"	""	"1, 2, 3"	""	"This section is entirely harzburgite with both granular and intersitital opx (13%), as well as trace clinopyroxene and Cr-spinel."	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic veins composed of prehnite, chlorite, and brown-stained clinopyroxene. The mesh is brown-black, bastites are black and green, and spinel displays a bronze color. The serpentine mesh texture is cut by a large number of fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	"weakly porphyroclastic serpentinized harzburgite with regular or weakly foliated mesh"	
"399"	"U1601"	"C"	"217"	"R"	"1"	""	"399-U1601C-217R-1"	"0.0"	"138.0"	"1065.800"	"1066.490"	"1067.180"	"1065.8"	"1066.49"	"1067.18"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mainly harzburgite with mostly granular orthopyroxene (15%), as well as trace clinopyroxene and Cr-spinel. The harzburgite is cut by pervasively altered gabbro veins. The lowermost 17 cm is an orthopyroxene-bearing dunite with trace spinel."	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic veins composed of a massive unidentified white mineral, chlorite, amphibole, prehnite, and secondary plagioclase. The mesh is brown-black and bastites are black and green. Spinel is fresh. The serpentine mesh texture is cut by a large number of fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	" weakly porphyroclastic serpentinized harzburgite"	
"399"	"U1601"	"C"	"217"	"R"	"2"	""	"399-U1601C-217R-2"	"0.0"	"136.0"	"1067.180"	"1067.860"	"1068.540"	"1067.18"	"1067.86"	"1068.54"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is harzburgite cut by two altered intervals of gabbro. The harzburgite averages 14% orthopyroxene and has trace Cr-spinel. "	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic veins composed of brown-stained clinopyroxene, amphibole, chlorite, and plagioclase. Highly altered gabbro (22-38 cm). Locally, along the rims of the magmatic veins, presence of oxides. The mesh is brown-black and the bastite are black. The serpentine mesh texture is cut by a large number of fibrous to massive chrysotile veins and picrolite veins that also cut the hydrothermally altered magmatic veins."	"patchy regular mesh"	
"399"	"U1601"	"C"	"217"	"R"	"3"	""	"399-U1601C-217R-3"	"0.0"	"147.0"	"1068.540"	"1069.275"	"1070.010"	"1068.54"	"1069.275"	"1070.01"	""	"1, 2, 3"	""	"This section is entirely harzburgite with both granular and intersitital opx (15%), as well as trace clinopyroxene and Cr-spinel."	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic veins composed of chlorite and amphibole.The mesh is brown-black. The bastites are preferentially black along the magmatic veins, otherwise, they are green. A black corona is present around orthopyroxene and bastite. Spinel is fresh. The serpentine mesh texture is cut by fibrous to massive chrysotile veins that vary in abundance, and picrolite veins that also cut the hydrothermally altered magmatic veins."	"weakly porphyroclastic serpentinized harzburgite with a weakly foliated to regular mesh"	
"399"	"U1601"	"C"	"218"	"R"	"1"	""	"399-U1601C-218R-1"	"0.0"	"141.0"	"1070.600"	"1071.305"	"1072.010"	"1070.6"	"1071.305"	"1072.01"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The top half of this section is orthopyroxene-bearing dunite with both granular and interstitial orthopyroxene and trace spinel. Below a reactive boundary at 80 cm is coarse grained gabbro that has been partially amphibolitized. The gabbroic interval has 10 cm scale finer-grained patches"	"Highly serpentinized harzburgite and variably altered olivine-gabbro in the lower half of the section. In the serpentinite, the mesh is brown-black and the bastites are black and green. A black corona is present around orthopyroxene and bastites. Spinel is fresh. The serpentine mesh texture is cut by fibrous to massive chrysotile veins. The gabbro is cut by amphibole, talc, and zeolite veins, and the extent of alteration in the gabbro is highest near the contact with the serpentinite. "	"weakly porphyroclastic and mesh foliated serpentinized harzburgite with a contact with gabbro with grain size contacts and grain size variations"	
"399"	"U1601"	"C"	"218"	"R"	"2"	""	"399-U1601C-218R-2"	"0.0"	"106.0"	"1072.010"	"1072.540"	"1073.070"	"1072.01"	"1072.54"	"1073.07"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Gabbro continues from the overlying section down to 36 cm. Below is largely harzburgite with c. 11 % orthopyroxene  and trace clinopyroxene and Cr-spinel. Medium and coarse-grained gabbroic veins cut the harzburgite."	"Highly altered gabbro at the top of the section and highly serpentinized harzburgite and Opx-bearing dunite below 38 cm. The gabbro is cut by amphibole, talc, and zeolite veins and the extent of alteration is highest near the contact with the serpentinite. The serpentinite is cut by hydrothermally altered magmatic veins that are made of plagioclase, reddish brown-stained clinopyroxene, amphibole, secondary plagioclase, chlorite, and prehnite. The mesh is brown-black, bastites are black and green, and a black corona is present around orthopyroxene and bastite. Locally relicts olivine are present and sulfides coat fractures in the serpentinite. The serpentine mesh texture is cut by massive to fibrous chrysotile veins, and picrolite veins cut the hydrothermally altered magmatic vein."	"protogranular serpentinized harzburgite with gabbroic intrusions and sharp undeformed contacts"	
"399"	"U1601"	"C"	"218"	"R"	"3"	""	"399-U1601C-218R-3"	"0.0"	"141.0"	"1073.070"	"1073.775"	"1074.480"	"1073.07"	"1073.775"	"1074.48"	""	"1, 2, 3, 4, 5, 6"	""	"Othopyroxene-bearing dunite with trace spinel down to 86 cm. Medium- to coarse-grained gabbros make up the rest of the section"	"Variably altered Ol-bearing gabbro and highly serpentinized Opx-bearing dunite cut by hydrothermally altered magmatic veins made of clinopyroxene, chlorite, and prehnite. Olivine in gabbro is altered to clays (?) and sulfide. The extent of alteration in gabbro is highest near the contact with the serpentinite. There, relicts olivine is present. Mesh is brown-black. Bastite is black and green. Spinel has a yellowish-brown stain (sulfides?). Amphibole, talc, and zeolite veins in gabbro. Serpentine, serpentine-magnetite, carbonate-sulfide, and hydrothermally altered magmatic veins are present in serpentine."	"protogranular serpentinized harzburgite in moderately dipping contact with gabbro, gabbro has grain size variations and local protomylonitic deformation and a short interval of serpentinized harzburgite "	
"399"	"U1601"	"C"	"218"	"R"	"4"	""	"399-U1601C-218R-4"	"0.0"	"73.0"	"1074.480"	"1074.845"	"1075.210"	"1074.48"	"1074.845"	"1075.21"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is medium to coarse-grained gabbro, with an interval at 29-34 cm of harzburgite with 10% orthopyroxene, trace clinopyroxene, and trace Cr-spinel."	"Variably altered gabbro that is cut by amphibole and zeolite veins with a layer of serpentinized dunite layer sandwiched between 28 and 34 cm. The serpentinized dunite has a brown mesh and black bastites. "	"Protomylonitic (45deg) to isotropic gabbro in contact with serp harz (20-30 deg) that is protogranular. "	
"399"	"U1601"	"C"	"219"	"R"	"1"	""	"399-U1601C-219R-1"	"0.0"	"149.5"	"1075.500"	"1076.247"	"1076.995"	"1075.5"	"1076.247"	"1076.995"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This section is medium to coarse-grained gabbro down to 126 cm. Harzburgite with 10% orthopyroxene, trace clinopyroxene, and trace Cr-spinel is below."	"Highly altered, locally oxide-bearing, gabbro, and highly serpentinized harzburgite at the bottom of the section (112-137 cm). The gabbro is cut by amphibole, talc-carbonate(?), and zeolite veins. The mesh is black and brown. Bastite is black to greenish grey. Spinel not observed. The serpentine mesh texture is cut by subparallel fibrous to massive chrysotile veins."	"deformed gabbro cut by undeformed leucogabbro, steeply dipping gabbro protomylonite, protogranular serpentinized harzburgite"	
"399"	"U1601"	"C"	"219"	"R"	"2"	""	"399-U1601C-219R-2"	"0.0"	"147.5"	"1076.995"	"1077.733"	"1078.470"	"1076.995"	"1077.733"	"1078.47"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is mostly harzburgite and orthopyroxene-bearing dunite with trace clinopyroxene and spinel. Pervasively altered gabbro veins are present at 97-117 cm."	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic vein composed of chlorite and minor amphibole. The mesh is brown and black, the bastites are black, and spinel has a yellowish luster (sulfides?). The serpentinite is coated by sulfides (pyrrhotite) in #3 (13-19 cm), forming slickensides along fractures. The serpentine mesh texture is cut by subparallel fibrous chrysotile veins, and picrolite veins cutting the hydrothermally altered magmatic vein."	"protogranular serpentinized harzburgite with a regular mesh"	
"399"	"U1601"	"C"	"219"	"R"	"3"	""	"399-U1601C-219R-3"	"0.0"	"82.0"	"1078.470"	"1078.880"	"1079.290"	"1078.47"	"1078.88"	"1079.29"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"The harzburgite from the previous section is at the top of this section down to 24.5 cm. Below is a coarse-grained granular gabbro."	"Highly serpentinized Cpx-bearing harzburgite at the top of the section (0-20 cm) and slightly altered gabbro. The gabbro is cut by talc-carbonate and zeolite veins. Close to the contact with the serpentinite, the gabbro is more altered (whitish aspect due to secondary plagioclase and minor prehnite, potentially chlorite/clays after clinopyroxene). In the serpentinite, the mesh is brown and black and the bastites are black. The serpentine mesh texture is cut by fibrous chrysotile veins."	"protogranular serpentinized harzburgite with a regular mesh, contact with gabbro with grain size variations"	
"399"	"U1601"	"C"	"220"	"R"	"1"	""	"399-U1601C-220R-1"	"0.0"	"128.0"	"1080.300"	"1080.940"	"1081.580"	"1080.3"	"1080.94"	"1081.58"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"From 0-58 cm is coarse-grained gabbronorite. The rest is coarse-grained gabbro with trace oxide bounded by shear zones with domains of granular hornblende diorite."	"Moderately altered gabbro that is cut by amphibole-secondary plagioclase, talc, and zeolite veins. The gabbro is more altered down section. Sulfides are locally associated with clays/chlorite after clinopyroxene. "	"gabbro isotropic, variable grain size, protmylonite interval"	
"399"	"U1601"	"C"	"221"	"R"	"1"	""	"399-U1601C-221R-1"	"0.0"	"150.0"	"1085.200"	"1085.950"	"1086.700"	"1085.2"	"1085.95"	"1086.7"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"From 0-48 cm is coarse-grained subophitic gabbro. The interval between 48 and 98 cm is oxide gabbro with sulfides. Below 98 cm is medium-grained gabbro with coarse-grained patches."	"Slightly altered gabbro and oxide gabbro that are cut by amphibole-chlorite, talc, and zeolite veins. Clinopyroxene is altered to amphibole, plagioclase is altered to chlorite and secondary plagioclase. Sulfides are associated with oxides in the oxide gabbro."	"gabbro isotropic, variable grain size, protmylonite interval"	
"399"	"U1601"	"C"	"221"	"R"	"2"	""	"399-U1601C-221R-2"	"0.0"	"151.0"	"1086.700"	"1087.455"	"1088.210"	"1086.7"	"1087.455"	"1088.21"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is coarse-grained granular to subophitic gabbro. "	"Slightly altered gabbro cut by amphibole veins, talc veins, veins composed of an unidentified white mineral, and zeolite veins. Clinopyroxene is altered to amphibole, plagioclase is altered to chlorite and secondary plagioclase. "	"gabbro, isotrpoic, variable grain size, undeformed"	
"399"	"U1601"	"C"	"221"	"R"	"3"	""	"399-U1601C-221R-3"	"0.0"	"147.0"	"1088.210"	"1088.945"	"1089.680"	"1088.21"	"1088.945"	"1089.68"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is mostly coarse-grained granular to subophitic gabbro. The lowest 14 cm is orthopyroxene-bearing dunite with trace Cr-spinel."	"Slightly altered gabbro and pebbles of highly serpentinized harzburgite at the bottom of the section. Locally patchy and halo alteration occurs along veins where clinopyroxene is altered to a mixture of clays and chlorite, and plagioclase is altered to prehnite. In the serpentinite, the mesh is brown-black and bastites are black. The gabbro contains talc-carbonate veins, zeolite veins and an amphibole-chlorite vein near the contact to the serpentinite. The highly serpentinized harzburgite contains fibrous to massive chrysotile veins and a mesh texture of variable thickness."	"gabbro, isotrpoic,  undeformed, with some protogranular serpentinized harzburgite rubble."	
"399"	"U1601"	"C"	"222"	"R"	"1"	""	"399-U1601C-222R-1"	"0.0"	"110.0"	"1090.000"	"1090.550"	"1091.100"	"1090"	"1090.55"	"1091.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"This section is intermingled peridotites and gabbroic rocks. The top 31cm is a continuation of orthopyroxene-bearing dunites from the overlying section. From 31 to 50 cm is coarse grained gabbro with medium grained olivine gabbro domains. The rest of the section is harzburgite with 10 % orthopyroxene (granular and interstitial) and trace chromium spinel with a few highly altered gabbroic veins."	"Highly serpentinized Opx-bearing dunite (mostly as pebbles) at the top and highly serpentinized harzburgite at the bottom of the section, with variably altered gabbro inbetween (55-60 cm). The highly serpentinized harzburgite is cut by hydrothermally altered magmatic veins composed of former clinopyroxene, chlorite, and amphibole, which itself is cut by picrolite veins. Chrysotile veins are fibrous to massive. The mesh is brown-black and the bastites are black and green. Spinel is fresh. The gabbro is slightly more altered at the bottom of the section and it is cut by amphibole and zeolite veins."	"Protogranular serp harz, reg mesh, with magmatic vein cut by ureverse faults. Isotropic gabbro interval."	
"399"	"U1601"	"C"	"222"	"R"	"2"	""	"399-U1601C-222R-2"	"0.0"	"132.0"	"1091.100"	"1091.760"	"1092.420"	"1091.1"	"1091.76"	"1092.42"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"The harzburgite from the overlying section continues through this section. The section has rare highly altered gabbro veins."	"Highly serpentinized harzburgite that is cut by hydrothermally altered magmatic veins of variable thickness. The altered magmatic veins are composed of brown-stained clinopyroxene, secondary plagioclase, chlorite, and amphibole, and are cut by picrolite veins. The mesh is brown-black and bastites are black and green. Spinel has a yellowish luster (sulfide?). The highly serpentinized harzburgite contains fibrous to massive, subparallel chrysotile veins and a mesh texture of variable thickness."	"Protogranular serp harz, reg mesh, with magmatic vein cut by ureverse faults."	
"399"	"U1601"	"C"	"223"	"R"	"1"	""	"399-U1601C-223R-1"	"0.0"	"150.0"	"1094.900"	"1095.650"	"1096.400"	"1094.9"	"1095.65"	"1096.4"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The upper 62 cm is dunite with orthopyroxene decresing and Cr-spinel increasing down section. Below are coarse-grained gabbronorite (62-106 cm) with granular to subophitic gabbro below."	"Highly serpentinized opx-bearing dunite and minor harzburgite at the top of the section and variably altered gabbro at the bottom half of the section. In the serpentinite, relicts of olivine are found. The mesh is brown-black and the bastites are mostly black and minor green. Spinel is fresh. The highly serpentinized harzburgite contains fibrous to massive, subparallel chrysotile veins and a mesh texture of variable thickness. The extent of alteration in the gabbro increases towards the upper contact with the serpentinite. The gabbro contains talc-carbonate-prehnite veins and zeolite veins."	"protogranular serp harz and dunite, reg to mod mesh (15deg), isotropic gabbro"	
"399"	"U1601"	"C"	"223"	"R"	"2"	""	"399-U1601C-223R-2"	"0.0"	"135.0"	"1096.400"	"1097.075"	"1097.750"	"1096.4"	"1097.075"	"1097.75"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The coarse gabbro from the overlying section continues."	"Slightly to moderately altered olivine-bearing gabbro. Olivine is mostly present at the bottom of the section where it is locally altered to clay and sulfides. Clinopyroxene is altered to chlorite and amphibole, and locally to a white unidentified mineral. The gabbro is cut by zeolite veins, amphibole-chlorite veins and one larger chlorite vein near the bottom of the section."	"gabbro, isotrpoic, regular mesh"	
"399"	"U1601"	"C"	"224"	"R"	"1"	""	"399-U1601C-224R-1"	"0.0"	"146.0"	"1099.700"	"1100.430"	"1101.160"	"1099.7"	"1100.43"	"1101.16"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The upper 52.5 cm is harzburgite with 10% granular and interstitial orthopyroxene and trace Cr-spinel. The rest of the section is coarse-grained granular to subophitic gabbronorite."	"Highly altered serpentinized harzburgite and opx-bearing dunite at the top of the section and slightly to locally highly altered gabbro towards the lower part of the section. The extent of serpentinization is variable, with locally olivine relicts being present. The mesh is mostly brown-black and contains finely disseminated sulfides, the bastites are black. The highly serpentinized harzburgite contains fibrous to massive, subparallel chrysotile veins and a mesh texture of variable thickness. In the gabbro, the extent of alteration increases at the contact with the serpentinite and along veins. The gabbro is cut by talc-carbonate and zeolite veins."	"Protogranular to porphyroclastic (15deg) serp harz, weak fol mesh (15deg) above isotropic gabbro with fractures and microfaults"	
"399"	"U1601"	"C"	"224"	"R"	"2"	""	"399-U1601C-224R-2"	"0.0"	"110.0"	"1101.160"	"1101.710"	"1102.260"	"1101.16"	"1101.71"	"1102.26"	""	"1, 2, 3, 4, 5, 6, 7"	""	"The first 51 cm continues the coarse-grained gabbronorite from the overlying section. Beneath the gabbro is harzburgite with 10% granular and interstitial orthopyroxene and trace Cr-spinel."	"Slightly to moderately altered gabbro at the top of the section and highly serpentinized harzburgite towards the bottom of the section. The gabbro is cut by prehnite and zeolite veins and contains sulfides. The highly serpentinized harzburgite contains fibrous to massive, subparallel chrysotile veins and a mesh texture of variable thickness. The mesh is brown-black and the bastites are black and green. "	"fractured isotropic gabbro above protogranular to porphyroclastic (20deg) serp harz, no mesh to mod mesh (20deg)"	
"399"	"U1601"	"C"	"225"	"R"	"1"	""	"399-U1601C-225R-1"	"0.0"	"144.0"	"1104.600"	"1105.320"	"1106.040"	"1104.6"	"1105.32"	"1106.04"	""	"1, 1, 2, 2, 3, 3, 4, 5, 6, 7"	""	"Most of this section is harzburgite with 15% mostly granular orthopyroxene and trace clinopyroxene and Cr-spinel. The interval between 88 and 99 cm is dunite."	"Highly serpentinized harzburgite and minor dunite. The extent of serpentinization is variable throughout the section with some relicts of olivine.  The mesh is brown-black and the bastites are grey-green. The serpentinite is cut by fibrous to massive chrysotile veins and a thick carbonate vein."	"protogranular to porphyroclastic serp harz and dunite with regular mesh - FRESH olivine kernels visible in mesh"	
"399"	"U1601"	"C"	"225"	"R"	"2"	""	"399-U1601C-225R-2"	"0.0"	"141.0"	"1106.040"	"1106.745"	"1107.450"	"1106.04"	"1106.745"	"1107.45"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This section is harzburgite with 15% mostly granular orthopyroxene and trace Cr-spinel and clinopyroxene. "	"Highly serpentinized harzburgite containing a brown and black mesh texture and grey-green bastites. The serpentinite is cut by fibrous chrysotile veins, a thick carbonate vein and a hydrothermally altered magmatic vein composed of secondary plagioclase and chlorite."	"porphyroclastic serp harz (0deg) with regular to weak fol (0-30deg) mesh - olivine kernels visible in mesh"	
"399"	"U1601"	"C"	"225"	"R"	"3"	""	"399-U1601C-225R-3"	"0.0"	"150.0"	"1107.450"	"1108.200"	"1108.950"	"1107.45"	"1108.2"	"1108.95"	""	"1, 2, 3"	""	"Most of this section is harzburgite with 11% mostly granular orthopyroxene and trace Cr-spinel. The lowest 7 cm is coarse-grained gabbro"	"Highly serpentinized harzburgite containing a brown-black mesh and grey-green and black bastites. The serpentinite is cut by fibrous chrysotile veins and a hydrothermally altered magmatic vein composed of secondary plagioclase and chlorite. At the bottom of the section moderately altered gabbro occurs in two pieces (rubble)."	"protogranular to porphyroclastic (10-15deg) serp harz, weak fol mesh (0-15deg)"	
"399"	"U1601"	"C"	"225"	"R"	"4"	""	"399-U1601C-225R-4"	"0.0"	"29.0"	"1108.950"	"1109.095"	"1109.240"	"1108.95"	"1109.095"	"1109.24"	""	"1, 2, 3"	""	"This section is coarse-grained gabbro continuing from the overlying section."	"Slightly altered gabbro that is cut by a chlorite-carbonate-prehnite vein and chlorite-amphibole veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"226"	"R"	"1"	""	"399-U1601C-226R-1"	"0.0"	"141.0"	"1109.400"	"1110.105"	"1110.810"	"1109.4"	"1110.105"	"1110.81"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"The section's top continues the coarse-grained gabbro from the overlying section. Below 35 cm, the gabbro becomes medium grained and has domains of hornblende diorite from 35-63 cm."	"Variably altered pegmatitic gabbro and diorite showing an increasing extent of alteration upsection and towards the veins. The gabbro is cut by talc-carbonate-prehnite veins, zeolite veins and amphibole veins."	"isotropic gabbro with strong facturing, microfaults and cataclasite 0-23cm."	
"399"	"U1601"	"C"	"226"	"R"	"2"	""	"399-U1601C-226R-2"	"0.0"	"112.0"	"1110.870"	"1111.430"	"1111.990"	"1110.87"	"1111.43"	"1111.99"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is medium grained granular gabbro with domains of medium-grained hornblende diorite."	"Slightly altered gabbro and olivine-bearing gabbro with chlorite and zeolite veins, and a massive amphibole vein."	"isotrpoic gabbro, fractures"	
"399"	"U1601"	"C"	"227"	"R"	"1"	""	"399-U1601C-227R-1"	"0.0"	"144.0"	"1114.300"	"1115.020"	"1115.740"	"1114.3"	"1115.02"	"1115.74"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Harzburgite with a 2 cm altered gabbro vein within diffuse contacts."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by hydrothermally altered magmatic veins. The serpentinite contains a black-brown mesh and green to locally black bastites, that are cut by subparallel fibrous to massive chrysotile veins. The hydrothermally altered magmatic veins range in size from 5 mm to 20 mm and are comprised of amphibole, chlorite, and secondary plagioclase, often showing a rodingite-like alteration. The altered magmatic veins are cut by sets of up to 1.5 mm thick picrolite veins."	"Protogranular serp harz cut by little white veins (15deg) and magmatic veins (65-70deg). "	
"399"	"U1601"	"C"	"227"	"R"	"2"	""	"399-U1601C-227R-2"	"0.0"	"126.0"	"1115.740"	"1116.370"	"1117.000"	"1115.74"	"1116.37"	"1117"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Harzburgite with a relatively high proporton of opx and a granular texture."	"Highly serpentinized dunite and harzburgite, cut by hydrothermally altered magmatic veins that are comprised of red-stained clinopyroxene. The serpentinite is cut by a set of subparallel fibrous to massive chrysotile veins that locally also form slickensides on piece ends."	"variable orientation of white veins. "	
"399"	"U1601"	"C"	"228"	"R"	"1"	""	"399-U1601C-228R-1"	"0.0"	"111.0"	"1119.100"	"1119.655"	"1120.210"	"1119.1"	"1119.655"	"1120.21"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Most of this section is orthopyroxene-bearing dunite  with both granular and interstitial orthopyroxene and trace spinel. The dunite is cut by domains of coarse-grained, ganular olivine gabbro."	"Highly serpentinized Opx-bearing dunite and harzburgite. The dunite is cut by hydrothermally altered magmatic veins composed of plagioclase, clinopyroxene, secondary plagioclase, prehnite, chlorite, and amphibole, that are up to 20 mm thick. In the serpentinite the mesh is black and brown and the bastites are green and black, and the groundmass is cut by fibrous chrysotile veins that are more abundant at the top of the section."	"protogranular tp porphyroclastic serp harz (15deg), reg to weak mesh (15deg), gabbro fractured and veined."	
"399"	"U1601"	"C"	"229"	"R"	"1"	""	"399-U1601C-229R-1"	"0.0"	"142.0"	"1124.000"	"1124.710"	"1125.420"	"1124"	"1124.71"	"1125.42"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The upper 53vcm of this section is orthopyroxene-bearing dunite with trace spinel and both granular and interstitial orthopyroxene. The dunite is cut by domains of coarse-grained, ganular olivine gabbro. Harzburgite with 18% orthopyroxene, more than trace clinopyroxene, and trace Cr-spinel makes up most of the rest of the section. A domain of coarse-grained gabbro is present below 115 cm."	"Highly serpentinized harzburgite and Opx-bearing dunite with a layer of troctolite near the top of the section and variably altered olivine-bearing gabbro at the bottom of the section. In the harzburgite and opx-bearing dunite some relicts of olivine are present. The extent of serpentinization is variable throughout the section. In the serpentinite the mesh is brown-black and the bastites are black, and the mesh texture is cut by fibrous to massive chrysotile veins. The variably altered olivine-bearing gabbro is cut by amphibole, chlorite and zeolite veins."	"protomylonitic serp harz (20deg) with reverse sense mantle fabric. gabbro intervals"	
"399"	"U1601"	"C"	"229"	"R"	"2"	""	"399-U1601C-229R-2"	"0.0"	"62.0"	"1125.420"	"1125.730"	"1126.040"	"1125.42"	"1125.73"	"1126.04"	""	"1, 2, 3, 4, 5, 6, 7"	""	"Most of this section is harzburgite with an average of 10% granular orthopyroxene. The proportion of orthopyroxene decreses towards the contact with gabbro. A coarse-grained granular gabbro domain with clinopyroxene crystals as wide as ~35 mm is found near the top and bottom of the section."	"Variably altered gabbro and moderately altered troctolite at the top of the section is followed by highly serpentinized harzburgite in the lower part of the section. The altered gabbro is cut by zeolite veins. The serpentinite is cut by hydrothermally altered magmatic veins that are composed of plagioclase, clinopyroxene, amphibole, secondary plagioclase, chlorite, prehnite, and disseminated sulfides. In the serpentinite the mesh is brown and black and the bastites are green and locally black, and the mesh texture is cut by rare chrysotile veins. The altered magmatic veins are cut by green picrolite veins up to 5 mm thick. "	"porphyroclastic (30deg) serp harz, reg to weak mesh (30deg)"	
"399"	"U1601"	"C"	"230"	"R"	"1"	""	"399-U1601C-230R-1"	"0.0"	"137.5"	"1128.800"	"1129.487"	"1130.175"	"1128.8"	"1129.487"	"1130.175"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This section is mixed peridotites and gabbroic rocks. The upper 12 cm continues the harzburgite from the overlying unit. A coarse-grained gabbro is below. The boundary between these units is troctolitic. Below 38 cm is orthopyroxene-bearing dunite with trace Cr-spinel. Below 130 cm is coarse-grained granular to subophitic gabbro with disseminated oxides and with grain sizes decreasing toward its upper contact. This gabbro has a mylonitic texture"	"This section is comprised of alternating intervals of highly serpentinized harzburgite and slightly altered gabbro. The uppermost 12 cm of the section comprises serpentinized harzburgite followed by a coarse-grained gabbro with a more troctolilitc composition at the boundary between these two intervals. Below 45 cm the section is dominated by serpentinized harzburgite that is cut by hydrothermally altered magmatic veins followed by minor slightly altered gabbro at the very bottom of the section. The hydrothermally altered magmatic veins are composed of brown stained clinopyroxene, chlorite, and minor amphibole, and are cut by picrolite veins. In the serpentinite the mesh is brown-black to grey and the bastites are mostly grey to green and locally black. The extent of alteration in the gabbro increases toward the serpentinite contact."	"protogranular to porhpyhroclastic (35deg) serp harz above gabbro and ox gabbro pmylon. GABBRO AT CONTACT IS NOT DEFORMED"	
"399"	"U1601"	"C"	"230"	"R"	"2"	""	"399-U1601C-230R-2"	"0.0"	"123.5"	"1130.175"	"1130.793"	"1131.410"	"1130.175"	"1130.793"	"1131.41"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"The top 12 cm is an oxide-bearing gabbro with a mylonitic texture. Below is a section is coarse-grained disseminated oxide gabbronorite with a mylonitic fabric."	"Moderately altered gabbro to oxide gabbro that is cut by zeolite veins. Sulfides are locally associated with oxides (40-48 cm)."	"gabbro mylonite continuous section, reverse sense"	
"399"	"U1601"	"C"	"231"	"R"	"1"	""	"399-U1601C-231R-1"	"0.0"	"150.0"	"1133.700"	"1134.450"	"1135.200"	"1133.7"	"1134.45"	"1135.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The top of this section has harzburgite pebbles that may be accidental. The rest of the section is coarse-grained, granular gabbro with disseminated oxide."	"Highly serpentinized harzburgite occurs mostly as smaller rubble pieces at the top of the section and is followed by moderately altered gabbro, which dominates this section. In the serpentinites the mesh is brown-black and bastites are green, and the mesh texture is cut by abundant fibrous to massive chrysotile veins. The moderately altered gabbro is cut by amphibole veins and locally sulfides are associated with oxides. "	"serp harz above weakly foliated to protomylonitic gabbro (30-70deg)"	
"399"	"U1601"	"C"	"231"	"R"	"2"	""	"399-U1601C-231R-2"	"0.0"	"133.0"	"1135.200"	"1135.865"	"1136.530"	"1135.2"	"1135.865"	"1136.53"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is medium-grained, granular gabbro with disseminated oxide."	"Slightly altered gabbro to oxide gabbro that is cut by a set of amphibole and zeolite veins. Locally sulfides are associated with oxides."	"weakly foliated to protomylontic (30-80deg) gabbro"	
"399"	"U1601"	"C"	"231"	"R"	"3"	""	"399-U1601C-231R-3"	"0.0"	"111.0"	"1136.530"	"1137.085"	"1137.640"	"1136.53"	"1137.085"	"1137.64"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This section is coarse-grained, granular gabbro with disseminated oxide. Its largest clinopyroxene crystal is ~45 mm across."	"Slightly altered gabbro to oxide gabbro that is cut by a set of amphibole and zeolite veins. Locally sulfides are associated with oxides."	"protomylonitic gabbro continuous deformation across section (40deg), reverse sense"	
"399"	"U1601"	"C"	"232"	"R"	"1"	""	"399-U1601C-232R-1"	"0.0"	"145.0"	"1138.500"	"1139.225"	"1139.950"	"1138.5"	"1139.225"	"1139.95"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is coarse-grained, granular gabbronorite with local zones of disseminated oxides. "	"Slightly altered gabbro to oxide gabbro that is cut by amphibole, talc, and zeolite veins, and locally sulfides occur associated with oxides. At the top of the section a few pebbles of variably serpentinized harzburgite occur that show a brown-black mesh texture."	"gabbro weakly foliated with coarse grained undeformed sections and some fracturing"	
"399"	"U1601"	"C"	"232"	"R"	"2"	""	"399-U1601C-232R-2"	"0.0"	"146.0"	"1139.950"	"1140.680"	"1141.410"	"1139.95"	"1140.68"	"1141.41"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"This section is coarse-grained, granular gabbronorite with local zones of disseminated oxides."	"Slightly altered gabbro to minor oxide gabbro that is cut by amphibole, talc, and zeolite veins, and locally sulfides occur associated with oxides. "	"protomylonitic to weakly foliated gabbro (25-45deg)"	
"399"	"U1601"	"C"	"232"	"R"	"3"	""	"399-U1601C-232R-3"	"0.0"	"99.0"	"1141.410"	"1141.905"	"1142.400"	"1141.41"	"1141.905"	"1142.4"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is coarse-grained, granular gabbronorite with trace oxide."	"Slightly altered gabbro that is cut by amphibole, talc, and zeolite veins. The extent of alteration increases down section."	"weakly folitaed gabbro with fractured grains                                                                                   "	
"399"	"U1601"	"C"	"233"	"R"	"1"	""	"399-U1601C-233R-1"	"0.0"	"150.0"	"1143.400"	"1144.150"	"1144.900"	"1143.4"	"1144.15"	"1144.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"This section is coarse-grained, granular gabbronorite with trace oxide."	"Variably altered gabbro showing a higher degree of hydrothermal alteration in the middle of the section. The altered gabbro is cut by amphibole and zeolite veins, and in one piece a fine-grained quartz-secondary plagioclase-prehnite vein."	"altered gabbro with mylonitic gabbroic vein"	
"399"	"U1601"	"C"	"233"	"R"	"2"	""	"399-U1601C-233R-2"	"0.0"	"151.0"	"1144.900"	"1145.655"	"1146.410"	"1144.9"	"1145.655"	"1146.41"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is coarse-grained, granular gabbronorite with trace oxide. Much of the section has a mylonitic fabric."	"Slightly to moderately altered and highly deformed gabbro to oxide-bearing gabbro that is cut by amphibole and zeolite veins. Locally disseminated primary sulfides (chalcopyrite, pyrrhotite) occur."	"gabbro mylontie with coarse grained and finer grained intervals - NORMAL SENSE"	
"399"	"U1601"	"C"	"234"	"R"	"1"	""	"399-U1601C-234R-1"	"0.0"	"144.5"	"1148.200"	"1148.922"	"1149.645"	"1148.2"	"1148.922"	"1149.645"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"This section is coarse-grained, granular gabbronorite with trace oxide. Much of the section has a mylonitic texture."	"Moderately altered and highly deformed gabbro to oxide-bearing gabbro that is cut by amphibole and zeolite veins. Locally sulfides are associated with oxides."	"gabbro mylonite (55deg) unclear shear sense, maybe normal"	
"399"	"U1601"	"C"	"234"	"R"	"2"	""	"399-U1601C-234R-2"	"0.0"	"145.5"	"1149.645"	"1150.372"	"1151.100"	"1149.645"	"1150.372"	"1151.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This section is coarse-grained, granular gabbro with trace oxide and orthopyroxene. Much of the section has a mylonitic texture."	"Moderately altered and deformed gabbro to oxide-bearing gabbro that is cut by amphibole and zeolite veins, and an amphibole vein associated with a pinkish, unidentified mineral. Locally, sulfides are associated with oxide."	"gabbro mylonite (75deg), mostly normal sense but some reverse sense"	
"399"	"U1601"	"C"	"234"	"R"	"3"	""	"399-U1601C-234R-3"	"0.0"	"88.5"	"1151.100"	"1151.543"	"1151.985"	"1151.1"	"1151.543"	"1151.985"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"This section is coarse-grained, granular gabbro with trace oxide and orthopyroxene. Much of the section has a mylonitic texture."	"Moderately altered and deformed gabbro that is cut by amphibole and zeolite veins."	"gabbro mylonite (80deg), mostly normal sense but some reverse sense"	
"399"	"U1601"	"C"	"235"	"R"	"1"	""	"399-U1601C-235R-1"	"0.0"	"125.0"	"1153.100"	"1153.725"	"1154.350"	"1153.1"	"1153.725"	"1154.35"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"The first bin is mixed pebbles of gabbro and serpentinized peridotites. Most if the section is orthopyroxene-bearing dunite with trace spinel. One coarse-grained gabbroic pebble is at c. 27 cm. Oxide gabbro veins infiltrate the lower dunite."	"Highly serpentinized Opx-bearing dunite that is cut by hydrothermally altered magmatic veins of variable thickness. The altered magmatic veins are comprised of red-stained clinopyroxene, plagioclase, chlorite, prehnite, and second plagioclase. At the very top of the section, pebbles of altered gabbro occur. In the serpentinite, the mesh is black to green and the bastites are grey, and the mesh texture is cut by some fibrous chrysotile veins. "	"Protogranular to porpyroclastic mantle fabric, undetermined serpentine foliation and an interval of isotropic gabbro.  Cross cut by two magmatic veins (0 and 40deg). "	
"399"	"U1601"	"C"	"236"	"R"	"1"	""	"399-U1601C-236R-1"	"0.0"	"123.0"	"1157.900"	"1158.515"	"1159.130"	"1157.9"	"1158.515"	"1159.13"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"The orthopyroxene-bearing dunite from the overlying section continues down to 4 cm. Disseminated oxide gabbro is between 4 and 12 cm. A ~25cm interval of harzburgite with high opx abundance and grain size is from 12 to 41 cm. The rest of the section is medium- to coarse-grained gabbro."	"Highly serpentinized Opx-bearing dunite and harzburgite cut by a thick, hydrothermally altered gabbroic vein near the top of the section. The serpentinite is followed by slightly to moderately altered gabbro toward the bottom of the section that shows a lower degree of alteration neard the contact with the serpentinite. The altered gabbro is cut by zeolite and amphibole veins. In the serpentinite, the mesh is black and grey and the bastites are greenish. Fibrous chrysotile veins cutting the mesh texture occur only rarely."	"Porphyroclastic mantle fabric (25deg), undertermined serpentine foliation, and gabbro intervals that are isotropic to strongly foliationed.  A set of amphibole veins (45deg)."	
"399"	"U1601"	"C"	"236"	"R"	"2"	""	"399-U1601C-236R-2"	"0.0"	"80.0"	"1159.130"	"1159.530"	"1159.930"	"1159.13"	"1159.53"	"1159.93"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"The upper half of this section is gabbro continuous from previous section The rest of the section is farzburgite with discrete gabbro veins."	"Moderately altered gabbro at the top of the section and highly serpentinized orthopyroxene-bearing dunite in the lower half of the section. The gabbro shows a higher degree of alteration near the contact with the serpentinite and is cut by amphibole and zeolite veins. The serpentinite is cut by hydrothermally altered magmatic veins that range in size from 2 mm to 10 mm and are comprised of red-stained clinopyroxene, amphiboles, chlorite, and prehnite. Massive to fibrous chrysotile veins of variable thickness locally cut the mesh texture of the serpentinite."	"Protogranular mantle fabric, undetermined serpentine foliation, and a protomylonitic gabbro interval.  Cut by two magmatic veins (45 and 55deg)."	
"399"	"U1601"	"C"	"237"	"R"	"1"	""	"399-U1601C-237R-1"	"0.0"	"150.0"	"1162.800"	"1163.550"	"1164.300"	"1162.8"	"1163.55"	"1164.3"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"The upper 97 cm is coarse-grained gabbronorite, with an interval of olivine gabbro from 17 to 24 cm. Below is dunite, underlain by harzburgite, both with more than trace amounts of spinel."	"Highly serpentinized Opx-bearing dunite at the top of the section and moderately to highly altered gabbro at the bottom of the section. The serpentinite is cut by hydrothermally altered magmatic veins that are comprised of red-stained clinopyroxene, amphibole, chlorite, and prehnite. The mesh of the serpentinite is grey-black and locally brownish, the bastites are grey and brown, and the serpentinite mesh texture is cut by fibrous to locally massive chrysotile veins. The gabbro is cut by amphibole and zeolite veins and the degree of alteration increases towards the contact with the serpentinite."	"Isotropic to strongly foliated gabbro and a protogranular mantle fabric in serpentinized harzburgite.  Cut by a steeply dipping magmatic vein. "	
"399"	"U1601"	"C"	"237"	"R"	"2"	""	"399-U1601C-237R-2"	"0.0"	"62.0"	"1164.300"	"1164.610"	"1164.920"	"1164.3"	"1164.61"	"1164.92"	""	"1, 2, 3, 4, 5, 6, 7"	""	"This section is orthopyroxene-bearing dunite with a coarse-grained olivine gabbro interval from 32 to 41 cm."	"Highly serpentinized Opx-bearing dunite that is cut by a thick hydrothermally altered magmatic vein. The altered magmatic vein is cut by picrolite vein and the serpentinite mesh texture is locally cut by fibrous chrysotile veins."	"Protogranular mantle fabric with isotropic gabbro intervals.  One gabbro-serp harz contact is dipping 20deg.  A sheared green vein is moderately dipping and has a normal offset."	
"399"	"U1601"	"C"	"238"	"R"	"1"	""	"399-U1601C-238R-1"	"0.0"	"150.0"	"1167.600"	"1168.350"	"1169.100"	"1167.6"	"1168.35"	"1169.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"The first bin is mixed gabbro and peridotite pebbels. The second bin is a cobble of troctolite. The rest of the section is orthopyroxene-bearing dunite grading downward to harzburgite, both with trace spinel. A gabbro intrusion hosted in the dunite."	"Highly serpentinized harzburgite and opx-bearing dunite that are cut by hydrothermally altered magmatic veins. The hydrothermally altered magmatic veins are composed of amphibole and chlorite and possibly talc, showing a rodingite-like alteration, and locally these veins are cut by green picrolite veins. The serpentinite has a green mesh texture and bastites are grey to greenish. Fibrous chrysotile veins cutting the mesh texture occur only very rarely."	"Protogranular to weakly porphyroclastic mantle fabric with undetermined serpentine foliation and an interval of isotropic gabbro.  Cut by two magmatic veins (45 and 75deg)."	
"399"	"U1601"	"C"	"238"	"R"	"2"	""	"399-U1601C-238R-2"	"0.0"	"146.0"	"1169.100"	"1169.830"	"1170.560"	"1169.1"	"1169.83"	"1170.56"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This section is a coarse-grained granular gabbro above 53 cm. The rest of the section is coarse-grained oxide gabbro."	" Moderately altered to variably deformed gabbro to oxide-gabbro that locally shows a high extent of alteration. The gabbro is cut by amphibole and zeolite veins and in places abundant sulfides occur as patches."	"Isotropic to protomylonitic gabbro with moderate dip."	
"399"	"U1601"	"C"	"238"	"R"	"3"	""	"399-U1601C-238R-3"	"0.0"	"130.0"	"1170.560"	"1171.210"	"1171.860"	"1170.56"	"1171.21"	"1171.86"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Gabbro to oxide gabbro with oxide proportion generally increasing down section."	"Highly to moderately altered gabbro and oxide gabbro that is cut by amphibole, chlorite and zeolite veins. Locally, sulfides occur disseminated in the groundmass."	"Isotropic to mylonitic gabbro with moderate to steep dips. "	
"399"	"U1601"	"C"	"239"	"R"	"1"	""	"399-U1601C-239R-1"	"0.0"	"147.0"	"1172.500"	"1173.235"	"1173.970"	"1172.5"	"1173.235"	"1173.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22"	""	"Fine grained oxide gabbro for the uppermost 6 cm. The rest is coarse-grained disseminated oxide gabbronorite."	"Moderately altered gabbro to oxide gabbro that is cut by amphibole and zeolite veins and locally contains abundant sulfides."	"Gabbro protomylonite with moderate dip."	
"399"	"U1601"	"C"	"239"	"R"	"2"	""	"399-U1601C-239R-2"	"0.0"	"144.0"	"1173.970"	"1174.690"	"1175.410"	"1173.97"	"1174.69"	"1175.41"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Coarse-grained disseminated oxide gabbronorite continued from the overlying section."	"Variably altered and deformed gabbro that is cut by amphibole and zeolite veins."	"Weakly foliated to protomylonitic gabbro with moderate dip."	
"399"	"U1601"	"C"	"239"	"R"	"3"	""	"399-U1601C-239R-3"	"0.0"	"111.0"	"1175.410"	"1175.965"	"1176.520"	"1175.41"	"1175.965"	"1176.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Coarse-grained disseminated oxide gabbronorite continued from the overlying section."	"Slightly to moderately altered and variably deformed gabbro that is cut by amphibole and zeolite veins. The extent of hydrothermal alteration and deformation decreases down section."	"Gabbro mylonite - gneissic foliation, above gabbro weak def/undef, above gabbro rubble with isotropic interval."	
"399"	"U1601"	"C"	"240"	"R"	"1"	""	"399-U1601C-240R-1"	"0.0"	"149.0"	"1177.300"	"1178.045"	"1178.790"	"1177.3"	"1178.045"	"1178.79"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Coarse-grained gabbronorite with trace oxide continued from the overlying section. "	"Moderately altered gabbro that is cut by a network of zeolite veins and locally contains disseminated sulfides."	"gabbro, undeformed with grain size variations"	
"399"	"U1601"	"C"	"240"	"R"	"2"	""	"399-U1601C-240R-2"	"0.0"	"144.0"	"1178.790"	"1179.510"	"1180.230"	"1178.79"	"1179.51"	"1180.23"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Coarse-grained gabbronorite with trace oxide continued from the overlying section. "	"Moderately altered gabbro that is cut by a network of zeolite veins and rare chlorite veins."	"gabbro protomylonite + undef gabbro with white, green, amp veins"	
"399"	"U1601"	"C"	"240"	"R"	"3"	""	"399-U1601C-240R-3"	"0.0"	"152.0"	"1180.230"	"1180.990"	"1181.750"	"1180.23"	"1180.99"	"1181.75"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Coarse-grained gabbronorite with trace oxide continued from the overlying section. "	"Variably altered gabbro that is cut by zeolite and amphibole veins. The extent of hydrothermal alteration is higher near the center of the section and locally disseminated sulfides are abundant."	"Isotropic gabbro with sheared magmatic vein"	
"399"	"U1601"	"C"	"242"	"R"	"1"	""	"399-U1601C-242R-1"	"0.0"	"109.0"	"1182.200"	"1182.745"	"1183.290"	"1182.2"	"1182.688"	"1183.177"	""	"1, 2, 3, 4, 5, 6, 7"	""	"An opx-bearing dunite pebble, which might be from the ghost core (241) and therefore not in situ, is at the top of the section. The rest is coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. "	"Moderately altered gabbro with one piece of highly serpentinized opx-bearing dunite at the top of the section. The gabbro is cut by amphibole-chlorite, and zeolite veins. The serpentinite is cut by fibrous serpentine veins."	"largely isotropic gabbro w small sect serp harz; multiple black veins + a magmatic vein, normal shear"	
"399"	"U1601"	"C"	"242"	"R"	"2"	""	"399-U1601C-242R-2"	"0.0"	"142.0"	"1183.290"	"1184.000"	"1184.710"	"1183.177"	"1183.813"	"1184.45"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. "	"Moderately altered gabbro that is cut by zeolite veins and contains disseminated sulfides."	"isotropic to strongly foliated gabbro with some black veins"	
"399"	"U1601"	"C"	"242"	"R"	"3"	""	"399-U1601C-242R-3"	"0.0"	"106.0"	"1184.710"	"1185.240"	"1185.770"	"1184.45"	"1184.925"	"1185.4"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15"	""	"Coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. A thin interval of oxide gabbronorite is at around 60cm."	"Variably, but mostly moderately altered gabbro. The extent of hydrothermal alteration in the gabbro increases towards the middle of the section. The gabbro is cut by zeolite and chlorite veins and locally contains disseminated sulfides."	"isotropic gabbro, protomylonite interval"	
"399"	"U1601"	"C"	"243"	"R"	"1"	""	"399-U1601C-243R-1"	"0.0"	"147.0"	"1185.400"	"1186.135"	"1186.870"	"1185.4"	"1186.135"	"1186.87"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. "	"Variably and moderately altered gabbro to oxide-bearing gabbro that is cut by zeolite and chlorite veins, and one prehnite vein in the lower part of the section."	"isotropic gabbro w vein size variations"	
"399"	"U1601"	"C"	"243"	"R"	"2"	""	"399-U1601C-243R-2"	"0.0"	"145.0"	"1186.870"	"1187.595"	"1188.320"	"1186.87"	"1187.595"	"1188.32"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. "	"Variably and moderately altered gabbro that is cut by zeolite and chlorite veins, and locally contains disseminated sulfides."	"isotropic gabbro w vein size variations"	
"399"	"U1601"	"C"	"243"	"R"	"3"	""	"399-U1601C-243R-3"	"0.0"	"120.0"	"1188.320"	"1188.920"	"1189.520"	"1188.32"	"1188.92"	"1189.52"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Coarse-grained, granular to subophitic, and opx-bearing gabbro with trace oxides. A few olivine grains are between 100 and 104 cm."	"Variably altered gabbro with generally moderate to high degrees of alteration. Highest degrees of alteration occur at an interval between 80 - 95 cm, where abundant prehnite occurs."	"isotropic gabbro w vein size variations"	
"399"	"U1601"	"C"	"244"	"R"	"1"	""	"399-U1601C-244R-1"	"0.0"	"151.0"	"1190.200"	"1190.955"	"1191.710"	"1190.2"	"1190.955"	"1191.71"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Fine-grained gabbro unit with scattered poikilitic cpx. Coarse-grained at 44-53 cm. Has a chilled margin against the orthopyroxene-bearing dunite, which makes up the core below 104 cm."	"Moderately to highly altered gabbro and highly serpentinized harzburgite at the very bottom of the section. The gabbro contains abundant chlorite and prehnite, and is cut by amphibole and zeolite veins. The serpentinite has a brown mesh and black bastites."	"gabbro and diabase, grain size variation with green-black (75deg) and a piece end fault with reverse sense of shear."	
"399"	"U1601"	"C"	"244"	"R"	"2"	""	"399-U1601C-244R-2"	"0.0"	"142.0"	"1191.710"	"1192.420"	"1193.130"	"1191.71"	"1192.42"	"1193.13"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Harzburgite with a gabbronorite vein at ~67 cm. Contains both interstitial and granular opx and trace spinel."	"Highly serpentinized harzburgite cut by hydrothermally altered magmatic veins. The altered magmatic veins are comprised of prehnite and red-stained clinopyroxene, and are cut by picrolite veins. The mesh texture is cut by fibrous chrysotile veins and locally contains disseminated sulfides (piece 10 A). One massive chrysotile vein occurs at an interval between 34-37 cm."	"protogranular serpentinized harzburgite with a foliated mesh, magmatic veins (75deg) and white veins (10-25deg). "	
"399"	"U1601"	"C"	"244"	"R"	"3"	""	"399-U1601C-244R-3"	"0.0"	"84.0"	"1193.130"	"1193.550"	"1193.970"	"1193.13"	"1193.55"	"1193.97"	""	"1, 2, 3, 4, 5"	""	"This section is harzburgite like that of the overlying section. The orthopyroxene content decreases down section."	"Highly serpentinized harzburgite showing a grey-black mesh and grey to brownish bastites. The mesh texture is only locally cut by few fibrous chrysotile veinlets."	"protogranular serpentinized harzburgite with a weakly to strongly foliated mesh (0-30deg) and magmatic veins (40-47deg) and a white vein (10deg)."	
"399"	"U1601"	"C"	"245"	"R"	"1"	""	"399-U1601C-245R-1"	"0.0"	"149.0"	"1195.100"	"1195.845"	"1196.590"	"1195.1"	"1195.845"	"1196.59"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"At 0-30 cm is a harzburgite with trace spinel. Opx-bearing dunite. Between 36 and 131 cm is coarse-grained granular gabbronorite with fine-grained zone close to the contact with the overlying harzburgite. A medium-grained oxide gabbro is below."	"Highly serpentinized opx-bearing dunite at the top of the section in contact with moderately altered gabbro and oxide gabbro toward the bottom of the section. The serpentinite contains one carbonate-sulfide vein. The gabbro is cut by a network of zeolite veins and a carbonate-serpentine vein, the extent of alteration increases towards the contact with the serpentinite, and in the oxide gabbro disseminated sulfides are abundant. "	"protogranular serpentinized harzburgite, weakly foliated mesh (15deg) with isotropic gabbro of different grain sizes. Contact preserved but not oriented."	
"399"	"U1601"	"C"	"245"	"R"	"2"	""	"399-U1601C-245R-2"	"0.0"	"46.0"	"1196.590"	"1196.820"	"1197.050"	"1196.59"	"1196.82"	"1197.05"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Medium-grained orthopyroxene-bearing gabbro with trace oxide."	"Moderately altered gabbro that is cut by chlorite and zeolite veins."	"weakly foliated gabbro (30deg)."	
"399"	"U1601"	"C"	"246"	"R"	"1"	""	"399-U1601C-246R-1"	"0.0"	"145.5"	"1199.900"	"1200.628"	"1201.355"	"1199.9"	"1200.628"	"1201.355"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"Medium-grained orthopyroxene-bearing gabbro with trace oxide, continued from the overlying section."	"Moderately to highly altered gabbro that is cut by zeolite, amphibole, amphibole-oxide, and talc-serpentine veins. Highest degrees of alteration occur at an interval between 41 and 60 cm."	"strongly foliated gabbro (30-60deg) with sheared magmatic vein (80deg) with normal sense of shear and green veins (60deg)."	
"399"	"U1601"	"C"	"246"	"R"	"2"	""	"399-U1601C-246R-2"	"0.0"	"150.0"	"1201.355"	"1202.105"	"1202.855"	"1201.355"	"1202.105"	"1202.855"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Medium-grained orthopyroxene-bearing gabbro with trace oxide, continued from the overlying section down to 11 cm. Medium-grained disseminated oxide gabbronorite and gabbronorite makes up the rest of the section"	"Moderately to highly altered and variably deformed gabbro that is cut by zeolite, amphibole and chlortie-amphibole veins."	"isotropic gabbro with a weakly foliated interval (60deg); discrete ultramylonite."	
"399"	"U1601"	"C"	"246"	"R"	"3"	""	"399-U1601C-246R-3"	"0.0"	"68.5"	"1202.860"	"1203.203"	"1203.545"	"1202.86"	"1203.203"	"1203.545"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"This section is coarse-grained gabbronorite."	"Moderately to highly altered gabbro that is cut by zeolite, amphibole, and amphibole-oxide veins."	"isotropic gabbro"	
"399"	"U1601"	"C"	"247"	"R"	"1"	""	"399-U1601C-247R-1"	"0.0"	"150.0"	"1204.800"	"1205.550"	"1206.300"	"1204.8"	"1205.55"	"1206.3"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. "	"Moderately altered gabbro that is cut by zeolite and amphibole-chlorite-prehnite veins. The degree of alteration locally increases along the amphibole-chlorite-prehnite veins."	"isotropic gabbro with green veins (10-55deg)."	
"399"	"U1601"	"C"	"247"	"R"	"2"	""	"399-U1601C-247R-2"	"0.0"	"133.0"	"1206.300"	"1206.965"	"1207.630"	"1206.3"	"1206.965"	"1207.63"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. "	"Moderately altered gabbro with prehnite, chlorite-amphibole (1-2 mm), and zeolite veins. The degree of alteration in the gabbro locally increases along prehnite veins."	"isotropic gabbro with green and white veins (35-55deg)."	
"399"	"U1601"	"C"	"247"	"R"	"3"	""	"399-U1601C-247R-3"	"0.0"	"79.5"	"1207.630"	"1208.027"	"1208.425"	"1207.63"	"1208.027"	"1208.425"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. "	"Moderately altered gabbro that is cut by zeolite and amphibole-chlorite (up to 2 mm) veins."	"isotropic gabbro with grain size variations, green veins (55-60deg)."	
"399"	"U1601"	"C"	"248"	"R"	"1"	""	"399-U1601C-248R-1"	"0.0"	"129.0"	"1209.600"	"1210.245"	"1210.890"	"1209.6"	"1210.245"	"1210.89"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. "	"Slightly to moderately altered gabbro that is cut by zeolite and chlorite-amphibole veins and locally contains disseminated sulfides."	"isotropic and weakly foliated gabbro with green vein (20deg)."	
"399"	"U1601"	"C"	"248"	"R"	"2"	""	"399-U1601C-248R-2"	"0.0"	"82.0"	"1210.890"	"1211.300"	"1211.710"	"1210.89"	"1211.3"	"1211.71"	""	"1, 2, 3, 4, 5, 6"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. Trace oxide is present."	"Slightly altered gabbro that is cut by zeolite veins and one prehnite-chlorite vein, and locally contains disseminated sulfides."	"gabbro isotropic with grain size variations."	
"399"	"U1601"	"C"	"248"	"R"	"3"	""	"399-U1601C-248R-3"	"0.0"	"119.0"	"1211.710"	"1212.305"	"1212.900"	"1211.71"	"1212.305"	"1212.9"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"This is a full section of coarse-grained poikilitic and granular gabbronorite. There are 2 to 3 cm sized cpx crystals spaced through the section. Trace sulfide is present."	"Slightly altered gabbro that is cut by zeolite and chlorite-amphibole veins, and locally contains disseminated sulfides."	"isotropic gabbro with grain size variation and green veins (50-60deg)."	
"399"	"U1601"	"C"	"249"	"R"	"1"	""	"399-U1601C-249R-1"	"0.0"	"128.0"	"1214.500"	"1215.140"	"1215.780"	"1214.5"	"1215.14"	"1215.78"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12"	""	"This is a full section of coarse-grained granular gabbronorite. There are 1 cm sized cpx crystals between 50 and 60 cm. "	"Slightly altered gabbro that is cut by zeolite and amphibole-chlorite veins, and locally contains disseminated sulfides."	"gabbro isotropic cut by a steeply dipping vein."	
"399"	"U1601"	"C"	"249"	"R"	"2"	""	"399-U1601C-249R-2"	"0.0"	"69.5"	"1215.780"	"1216.128"	"1216.475"	"1215.78"	"1216.128"	"1216.475"	""	"1, 2, 3, 4, 5"	""	"This is a full section of coarse-grained granular gabbronorite. "	"Slightly altered gabbro that is cut by zeolite and amphibole-chlorite veins, and locally contains disseminated sulfides."	"gabbro isotropic with grain size variation cut by a steeply dipping green-black vein."	
"399"	"U1601"	"C"	"249"	"R"	"3"	""	"399-U1601C-249R-3"	"0.0"	"104.0"	"1216.475"	"1216.995"	"1217.515"	"1216.475"	"1216.995"	"1217.515"	""	"1, 2, 3, 4"	""	"This is a full section of coarse-grained granular gabbronorite. "	"Slightly altered gabbro that is cut by zeolite and amphibole-chlorite veins, and locally contains disseminated sulfides."	"gabbro isotropic, white and green veins"	
"399"	"U1601"	"C"	"249"	"R"	"4"	""	"399-U1601C-249R-4"	"0.0"	"114.5"	"1217.515"	"1218.088"	"1218.660"	"1217.515"	"1218.088"	"1218.66"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"This section is a full section of coarse-grained granular gabbronorite. Appears to be more seriate than other sections of this core, as it has cm-scale clinopyroxene crystals near the top of the section. "	"Slightly altered gabbro that is cut by a network of zeolite veins, and locally contains disseminated sulfides."	"gabbro isotropic"	
"399"	"U1601"	"C"	"250"	"R"	"1"	""	"399-U1601C-250R-1"	"0.0"	"150.0"	"1219.300"	"1220.050"	"1220.800"	"1219.3"	"1220.05"	"1220.8"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21"	""	"Fine-grained grading downwawrd to medium-grained equigranular granular gabbronorite."	"Variably and slighty altered gabbro that is cut by zeolite and amphibole-plagioclase veins. The degree of alteration increases towards hydrothermal veins and where alteration is highest amphibole, secondary plagioclase, and chlorite are abundant. Amphibole veins up to 1-2 mm wide are abundant in highly altered intervals."	"gabbro with magmatic spo and different grain sizes cut by steeply dipping magmatic vein."	
"399"	"U1601"	"C"	"250"	"R"	"2"	""	"399-U1601C-250R-2"	"0.0"	"140.5"	"1220.800"	"1221.503"	"1222.205"	"1220.8"	"1221.503"	"1222.205"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Medium-grained equigranular granular gabbronorite continuous from previous section. A few pieces have coarse-grained pyroxenes at 100-130 cm."	"Moderately altered gabbro cut by zeolite and chlorite-amphibole veins."	"weakly foliated to mylonitic gabbro (20-30deg)."	
"399"	"U1601"	"C"	"251"	"R"	"1"	""	"399-U1601C-251R-1"	"0.0"	"145.0"	"1224.200"	"1224.925"	"1225.650"	"1224.2"	"1224.925"	"1225.65"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Medium-grained equigranular granular gabbronorite continuous from overlying section. An interval of fine-grained gabbro is between 128.5 and 142 cm."	"Slightly altered gabbro that is cut by zeolite, prehnite-chlorite, and chlorite-amphibole veins. The degree of alteration is locally higher and locally disseminated sulfides occur in the groundmass."	"gabbro coarse grained isotropic with ultramylonite rubble and fine grained gabbro with magmatic SPO and isotropic intervals. "	
"399"	"U1601"	"C"	"251"	"R"	"2"	""	"399-U1601C-251R-2"	"0.0"	"94.0"	"1225.650"	"1226.120"	"1226.590"	"1225.65"	"1226.12"	"1226.59"	""	"1, 2, 3, 4"	""	"Medium-grained equigranular granular gabbronorite continuous from overlying section. An interval of medium-grained hornblende diorite is between 29 and 31 cm."	"Slightly altered gabbro that is cut by zeolite, chlorite-amphibole, chlorite-talc and a hydrothermally altered magmatic (dioritic) vein."	"isotropic gabbro with grain size variations and a sheared magmatic vein (30deg)."	
"399"	"U1601"	"C"	"251"	"R"	"3"	""	"399-U1601C-251R-3"	"0.0"	"138.0"	"1226.590"	"1227.280"	"1227.970"	"1226.59"	"1227.28"	"1227.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Medium- to coarse-grained equigranular granular gabbronorite continuous from overlying section. An interval of gine-grained gabbro is between 6 and 27 cm."	"Slightly altered gabbro that is cut by a network of zeolite veins, amphibole-chlorite and chlorite-prehnite veins."	"isotropic gabbro w grain size variations (15-30deg) and several green and black veins (35-70deg)."	
"399"	"U1601"	"C"	"251"	"R"	"4"	""	"399-U1601C-251R-4"	"0.0"	"93.5"	"1227.970"	"1228.438"	"1228.905"	"1227.97"	"1228.438"	"1228.905"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9"	""	"Coarse-grained granular gabbronorite."	"Slightly altered gabbro that is cut by amphibole and a network of zeolite veins."	"isotropic gabbro with black and green veins (20-55deg)."	
"399"	"U1601"	"C"	"252"	"R"	"1"	""	"399-U1601C-252R-1"	"0.0"	"135.0"	"1229.000"	"1229.675"	"1230.350"	"1229"	"1229.675"	"1230.35"	""	"1, 2, 3, 4, 5, 6"	""	"Medium-grained grading down to coarse-grained granular gabbronorite."	"Slightly altered gabbro that is cut by chlorite, a network of zeolite veins, and one large prehnite vein. Locally disseminated sulfides occur in the groundmass of the gabbro."	"gabbro isotropic with grain size variation; a magmatic vein (45deg)."	
"399"	"U1601"	"C"	"252"	"R"	"2"	""	"399-U1601C-252R-2"	"0.0"	"147.0"	"1230.350"	"1231.085"	"1231.820"	"1230.35"	"1231.085"	"1231.82"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Coarse-grained grading down to medium-grained granular gabbronorite."	"Slightly altered gabbro that is cut by a network of zeolite veins."	"gabbro isotropic with grain size variation, steeply dipping white vein. "	
"399"	"U1601"	"C"	"252"	"R"	"3"	""	"399-U1601C-252R-3"	"0.0"	"129.0"	"1231.820"	"1232.465"	"1233.110"	"1231.82"	"1232.465"	"1233.11"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Coarse-grained granular gabbronorite. "	"Slightly altered gabbro that is cut by a ntework of zeolite veins and one amphibole vein 1 mm in width."	"gabbro isotropic with grain size variation; and black veins (20-55deg)."	
"399"	"U1601"	"C"	"253"	"R"	"1"	""	"399-U1601C-253R-1"	"0.0"	"87.0"	"1233.900"	"1234.335"	"1234.770"	"1233.9"	"1234.335"	"1234.77"	""	"1, 2, 3, 4, 5"	""	"Coarse-grained, seriate, and granular gabbronorite, continuous from previous section. Largest cpx grain 20 mm."	"Slightly altered gabbro that is cut by a network of zeolite veins and locally contains disseminated sulfides."	"isotropic gabbro with sub-horizontal and moderately dipping white and green veins"	
"399"	"U1601"	"C"	"253"	"R"	"2"	""	"399-U1601C-253R-2"	"0.0"	"146.0"	"1234.820"	"1235.550"	"1236.280"	"1234.82"	"1235.55"	"1236.28"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Coarse-grained, seriate, and granular gabbronorite, continuous from previous section. Largest cpx grain 15 mm."	"Slightly to moderately altered gabbro that is cut by chlorite, prehnite-talc, amphibole, and a network of zeolite veins."	"isotropic gabbro w grain size variations, magmatic veins (30-60deg), and green veins (65-55deg)."	
"399"	"U1601"	"C"	"253"	"R"	"3"	""	"399-U1601C-253R-3"	"0.0"	"145.0"	"1236.280"	"1237.005"	"1237.730"	"1236.28"	"1237.005"	"1237.73"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24"	""	"Coarse-grained, seriate, and granular gabbronorite at the top and bottom. From 29 to 111 cm is a medium-grained, seriate, and granular gabbronorite."	"Slightly to moderately altered gabbro that is cut by prehnite-talc, amphibole, epidote and a network of zeolite veins."	"isotropic gabbro w grain size variations and veins"	
"399"	"U1601"	"C"	"254"	"R"	"1"	""	"399-U1601C-254R-1"	"0.0"	"150.0"	"1238.700"	"1239.450"	"1240.200"	"1238.7"	"1239.45"	"1240.2"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19"	""	"Coarse-grained, seriate, and granular gabbronorite. Largest cpx grain 20 mm. Grades downward to medium grained and more equigranular gabbronorite."	"Slightly to locally moderately altered gabbro that is cut by amphibole and zeolite veins, and one thick prehnite-epidote-chlorite vein."	"isotropic to strongly foliated gabbro cut by a moderately dipping magmatic vein."	
"399"	"U1601"	"C"	"254"	"R"	"2"	""	"399-U1601C-254R-2"	"0.0"	"144.0"	"1240.200"	"1240.920"	"1241.640"	"1240.2"	"1240.92"	"1241.64"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17"	""	"Medium-grained granular gabbronorite continues from the overlying section. It is underlain by coarse-grained, granular gabbronorite. There are a few 1-2 cm scale cpx crystals scattered through the section."	"Moderately altered gabbro that is cut by a network of zeolite veins."	"weakly foliated (25-55deg) to isotropic gabbro with grain size variation"	
"399"	"U1601"	"C"	"254"	"R"	"3"	""	"399-U1601C-254R-3"	"0.0"	"25.0"	"1241.640"	"1241.765"	"1241.890"	"1241.64"	"1241.765"	"1241.89"	""	"1, 2, 3"	""	"Coarse-grained, seriate, and granular gabbronorite. The argest cpx grain is 10 mm across."	"Slightly altered gabbro that is cut by zeolite and one chlorite-epidote-prehnite vein. The gabbro contains rare dissemniated sulfides in the groundmass."	"isotropic gabbro"	
"399"	"U1601"	"C"	"255"	"R"	"1"	""	"399-U1601C-255R-1"	"0.0"	"150.0"	"1243.600"	"1244.350"	"1245.100"	"1243.6"	"1244.35"	"1245.1"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Coarse-grained, seriate, and granular gabbronorite. The largest cpx grain is c. 20 mm across. Grain size variable but overall decreases down section."	"Slightly to moderately altered gabbro that is cut by carbonate-serpentine, zeolite and two thick prehnite-epidote veins up to 15 mm in size.The degree of alteration decreases from top to bottom and hydrothermal alteration is locally more pronounced close to the veins. "	"isotropic gabbro w magmatic (65deg) and black veins (10deg)."	
"399"	"U1601"	"C"	"255"	"R"	"2"	""	"399-U1601C-255R-2"	"0.0"	"130.5"	"1245.100"	"1245.753"	"1246.405"	"1245.1"	"1245.753"	"1246.405"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Coarse-grained irregularly grading downward to medium-grained, seriate, and granular gabbronorite. The largest cpx grain is c. 20 mm across near the top and 10 cm below. The basal 15 cm returns to coarse-grained gabbronorite."	"Slightly altered gabbro that is cut by zeolite, prehnite-epidote-carbonate, and chlorite-prehnite veins up to 10 mm in width."	"isotropic gabbro w few veins, moderately to steeply dipping."	
"399"	"U1601"	"C"	"255"	"R"	"3"	""	"399-U1601C-255R-3"	"0.0"	"89.5"	"1246.405"	"1246.852"	"1247.300"	"1246.405"	"1246.852"	"1247.3"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10"	""	"Medium-grained, seriate, and granular gabbronorite. The largest cpx is 10 cm across."	"Slightly altered gabbro that is cut by zeolite and chlorite veins, and two prehnite veins. Locally disseminated sulfides occur in the groundmass of the gabbro."	"isotropic gabbro with some grain size variations and sheared magmatic vein (50deg)."	
"399"	"U1601"	"C"	"256"	"R"	"1"	""	"399-U1601C-256R-1"	"0.0"	"144.0"	"1248.400"	"1249.120"	"1249.840"	"1248.4"	"1249.12"	"1249.84"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20, 21"	""	"Coarse-grained, seriate, and granular gabbronorite. A mm-scale trondhjemite vein runs through much of the length of this section."	"Slightly altered gabbro that is cut by zeolite veins and a thick prehnite-chlorite-epidote vein of 20 mm width. The prehnite-chlorite-epidote vein is cut by a chlorite-serpentine vein."	"isotropic gabbro with grain size variation, a weak shape preferred orientation, magmatic (15deg), and magmatic veins (55deg) and a green white vein (35deg)."	
"399"	"U1601"	"C"	"256"	"R"	"2"	""	"399-U1601C-256R-2"	"0.0"	"130.0"	"1249.840"	"1250.490"	"1251.140"	"1249.84"	"1250.49"	"1251.14"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14"	""	"Medium- to coarse-grained gabbronorite with varying textures. The largest cpx grains are c. 30 mm across."	"Slightly altered gabbro that is cut by amphibole and zeolite veins, and a prehnite-chlorite-epidote vein that is of potential magmatic origin and occurs along the edge of two pieces (pieces 7 and 8). The extent of hydrothermal alteration locally increases towards the prehnite-chlorite-epidote vein."	"coarse and fine grained isotropic gabbro with grain size contact (10deg). Cut by a magmatic vein (35deg) and a white vein (50deg)."	
"399"	"U1601"	"C"	"256"	"R"	"3"	""	"399-U1601C-256R-3"	"0.0"	"75.0"	"1251.140"	"1251.515"	"1251.890"	"1251.14"	"1251.515"	"1251.89"	""	"1, 2, 3, 4, 5, 6, 7, 8"	""	"Medium-grained grading downward to coarse-grained granular gabbronorite There are a cm scale cpx crystals scattered through the section. The largest is c. 30 mm across."	"Slightly altered gabbro that is cut by zeolite and chlorite-amphibole veins. The extent of hydrothermal alteration increases next to a vein."	"gabbro fine grain coarsening downwards cut by moderately dipping green and black veins."	
"399"	"U1601"	"C"	"257"	"R"	"1"	""	"399-U1601C-257R-1"	"0.0"	"149.0"	"1253.300"	"1254.045"	"1254.790"	"1253.3"	"1254.045"	"1254.79"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13"	""	"Coarse- to medium-grained gabbronorite with a trondhjemite domain in the lowermost 26 cm."	"Slightly to moderately altered gabbro that is cut by zeolite and chlorite-amphibole veins and one hydrothermally altered magmatic vein comprised of prehnite and epidote of 50 mm width."	"isotropic grabbro, grain size variation, magmatic veins have gentle to steep dips, a white vein has moderate dip."	
"399"	"U1601"	"C"	"257"	"R"	"2"	""	"399-U1601C-257R-2"	"0.0"	"136.0"	"1254.790"	"1255.470"	"1256.150"	"1254.79"	"1255.47"	"1256.15"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Coarse-grained, seriate, and granular gabbronorite."	"Slightly to moderately altered gabbro cut by zeolite and prehnite-chlorite-epidote veins."	"isotropic gabbro, grain size variation, one magmatic vein (60deg) and one white vein (65deg)."	
"399"	"U1601"	"C"	"257"	"R"	"3"	""	"399-U1601C-257R-3"	"0.0"	"92.0"	"1256.150"	"1256.610"	"1257.070"	"1256.15"	"1256.61"	"1257.07"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11"	""	"Coarse-grained, seriate, and granular gabbronorite."	"Slightly to moderately altered gabbro that is cut by zeolite and prehnite-chlorite-epidote veins that are likely of magmatic origin."	"isotropic gabbro, grain size variation, w magmatic veins, sheared, and magmatic breccias."	
"399"	"U1601"	"C"	"258"	"R"	"1"	""	"399-U1601C-258R-1"	"0.0"	"152.0"	"1258.100"	"1258.860"	"1259.620"	"1258.1"	"1258.86"	"1259.62"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18, 19, 20"	""	"Generally, a coarse-grained, seriate, and granular gabbronorite. A fine-grained interval of gabbronorite is between 15 and 19 cm."	"Slightly to moderately altered gabbro that is cut by zeolite, composite amphibole-serpentine veins, and chlorite-prehnite veins that are potentially of magmatic origin. The overall extent of alteration of the gabbro is moderate."	"gabbro with grain size variation, protomylonite with moderate dip.  Moderately dipping magmatic vein, as well as shallow and moderately dipping white and green veins."	
"399"	"U1601"	"C"	"258"	"R"	"2"	""	"399-U1601C-258R-2"	"0.0"	"135.0"	"1259.620"	"1260.295"	"1260.970"	"1259.62"	"1260.295"	"1260.97"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Coarse- to medium-grained gabbronorite with a tonalite domain in the uppermost 32 cm."	"Moderately altered gabbro that is cut by zeolite, chlorite-epidote, and one amphibole-chlorite-quartz vein. Locally the gabbro contains disseminated sulfides (pieces 10 and 12A)."	"isotropic, weakly foliated, and protomylonitic gabbro w magmatic vein (55deg) and a black sheared vein (20deg)."	
"399"	"U1601"	"C"	"259"	"R"	"1"	""	"399-U1601C-259R-1"	"0.0"	"135.0"	"1263.000"	"1263.675"	"1264.350"	"1263"	"1263.675"	"1264.35"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16, 17, 18"	""	"Coarse-grained, seriate, and granular gabbronorite continued from the overlying section."	"Moderately altered gabbro that is cut by zeolite veins."	"gabbro isotropic, a magmatic vein"	
"399"	"U1601"	"C"	"259"	"R"	"2"	""	"399-U1601C-259R-2"	"0.0"	"129.0"	"1264.350"	"1264.995"	"1265.640"	"1264.35"	"1264.995"	"1265.64"	""	"1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 15, 16"	""	"Medium-grained, seriate, and granular gabbronorite with a coarse-grained interval between 86 and 109 cm. A few cm scale cpx crystals are scattered through the section."	"Moderately altered gabbro that is cut by zeolite veins and one prehnite vein. The extent of hydrothermal alteration is variable and pyroxene is generally less altered. Higher degree of alteration in piece 7 and plagioclase is almost entirely replaced by prehnite and chlorite, while clinopyroxene is locally highly altered to amphibole."	"gabbro isotropic with grain size variability, moderate dip, cut by a moderately dipping white vein."