Figure F152 (continued). I. Aligned plagioclase exhibiting a primary magmatic fabric alignment surrounded by grains of dynamically recrystallized plagioclase (Sample 304-U1309D-30R-1, 55–58 cm) (cross-polarized light; FOV = 8 mm). J. Steeply dipping contact of gabbro intruding troctolite showing some crystal-plastic deformation (interval 304-1309D-8R-2, 20–29 cm). K. Localized deformation zone between more olivine rich gabbro deformed crystal plastically and less intensely strained gabbro (Sample 304-U1309D-8R-2, 26–28 cm) (plane-polarized light; FOV = 4 mm). L. Recrystallized pyroxene and plagioclase cut by a fracture filled with oxides; fracture was possibly coeval with dynamic recrystallization (Sample 304-U1309D-44R-2, 106–109 cm) (cross-polarized light; FOV = 8 mm).
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