Figure F152 (continued). E. Microgabbro intruding coarser grained gabbro across this transitional contact (interval 304-U1309D-62R-1, 81–93 cm). A leucocratic dikelet cuts both units. F. Magmatic foliation defined by aligned plagioclase feldspar (interval 304-U1309D-66R-2, 10–21 cm). G. Coarse-grained, plagioclase-rich gabbro intrudes serpentinite without related deformation (interval 304-U1309D-64R-2, 4–18 cm). H. Coarse-grained gabbro is intensely strained, producing a mylonite with mixed pyroxene, feldspar and plagioclase, along with a xenolith of an ultramafic rock (interval 304-U1309D-64R-2, 41–49 cm).
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