Figure F131. A. Fractures radiating into adjacent plagioclase grain from serpentinized olivine (Sample 305-U1309D-82R-2, 110–112 cm) (cross-polarized light; magnification = 2.5×). B. Fractures extending between serpentinized olivine grains through adjacent plagioclase grains (Sample 305-1309D-232R-1, 102–105 cm) (plane-polarized light; magnification = 10×).
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