Figure F158. A. Equilibrated plagioclase next to poikilitic clinopyroxene in troctolite (Sample 305-U1309D-112R-2, 67–70 cm) (cross-polarized light; field of view [FOV] = 1.37 mm). B. Well-equilibrated plagioclase crystals are present in an undeformed clinopyroxene oikocryst (Sample 305-U1309D-160R-2, 133–135 cm) (cross-polarized light; FOV = 5.5 mm). C. Plagioclase grains are enclosed by a continuous rim of clinopyroxene (Sample 305-U1309D-251R-1, 74–77 cm) (cross-polarized light; FOV = 5.5 mm). This association is trapped within an oikocrystic olivine grain. D. Plagioclase within poikilitic clinopyroxene grain (Sample 305-U1309D-94R-2, 27–30 cm) (cross-polarized light; FOV = 5.5 mm). E. Two prismatic plagioclase grains enclosed by clinopyroxene oikocryst (Sample 305-U1309D-184R-3, 50–53 cm) (cross-polarized light; FOV = 5.5 mm). F. Dunitic troctolite, showing only subtly misoriented grains of olivine separated by continuous plagioclase grain (Sample 305-U1309D-248R-2, 7–9 cm) (FOV = 5.5 mm). (Continued on next page.)
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