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Table T9. Modal proportions for grain mounts, Hole U1415J.

Mineral 345-U1415J-2G-Sand, TS 27 345-U1415J-2G-Sand, TS 28 Mean mode
Modal
(%)
Reconstructed
igneous mode
Modal
(%)
Reconstructed
igneous mode
Plagioclase 23.8 57.1 27.6 63.1 25.7
Pyroxene 13.0 31.6 10.3 25.1 11.7
Amphibole after pyroxene 14.7   10.1   12.4
Polycrystalline amphibole 3.5   3.1   3.3
Secondary plagioclase 8.7   7.8   8.2
Zeolite (including veins and plagioclase replacement) 2.9   3.7   3.3
Cataclasite 8.5   11.1   9.8
Bruised grain of plagioclase or pyroxene 0.0   0.2   0.1
Prehnite vein/Prehnite replacing cataclasite 1.7   1.7   1.7
Prehnite replacing plagioclase 2.9   2.3   2.6
Chlorite 8.7   9.3   9.0
Olivine 0.2 11.3 0.6 11.8 0.4
Clay 5.4   5.2   5.3
Epidote 1.7   1.2   1.4
Carbonate 0.2   0.2   0.2
Serpentine 0.0   0.4   0.2
Volcanic clasts 4.1   5.2   4.7
          0.0
Cataclastic (excluding volcanics, including prehnite
replacing cataclasite)
10.6   13.7   12.2
Altered phases 52.5   47.5   50.0
Prehnite 4.6   4.1   4.3

Igneous mode is estimated according to the following formula: plagioclase = plagioclase + secondary plagioclase + zeolite + prehnite + (cataclasite + bruised grains) × 0.7 + chlorite × 0.8 + epidote + carbonate; pyroxene (includes some orthopyroxene) = pyroxene + amphibole after pyroxene + (cataclasite + bruised grains) × 0.3; olivine = olivine + clay minerals + serpentine + polycrystalline amphibole + chlorite × 0.2. TS = thin section.

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