Figure F192 (continued). D. Troctolite with moderate intensity of serpentine foliation dipping steeply (Sample 305-U1309D-110R-3, 79–92 cm). Later fault veins with subhorizontal talc fibers are present subparallel to the serpentine foliation. E. Weak serpentine foliation dipping steeply in troctolite (Sample 305-U1309D-111R-4, 0–27 cm). Earlier thin magmatic veins are crosscut by the serpentine foliation. F. Steeply dipping serpentine foliation in troctolite, crosscutting earlier magmatic veins (Sample 305-U1309D-112R-2, 53–71 cm).
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