Figure F29. Scans of oversized thin sections from two intervals of deformed rock given by the red dots in Figure F28. A. Sample 176-735B-147R-6 (Piece 2A, 45-51 cm), gneissic gabbro, lithologic Interval 710. B. Sample 176-735B0148R-1 (Piece 3B, 127-132 cm), porphyroclastic oxide gabbro. Both sections are oriented in the same way with arrows pointing toward the top of the core. Note the darker clinopyroxene (gray) and greater abundance of oxide minerals (black) in B than in A. C, D. The oxides from the two respective thin sections of A and B are selected (black). Alignment of oxides along planes of foliation is evident in both.

Figure F29. Scans of oversized thin sections from two intervals of deformed rock given by the red dots in Figure F28. A. Sample 176-735B-147R-6 (Piece 2A, 45-51 cm), gneissic gabbro, lithologic Interval 710. B. Sample 176-735B0148R-1 (Piece 3B, 127-132 cm), porphyroclastic oxide gabbro. Both sections are oriented in the same way with arrows pointing toward the top of the core. Note the darker clinopyroxene (gray) and greater abundance of oxide minerals (black) in B than in A. C, D. The oxides from the two respective thin sections of A and B are selected (black). Alignment of oxides along planes of foliation is evident in both.