Fig. 42
From: The Atlantis Bank Gabbro Massif, Southwest Indian Ridge
MODE 2000 Kaiko 10K ROV Dives 173 and 174 (Fig. 3) showing a split traverse from the base of the eastern transform wall at ~ 5000 m to the detachment fault surface at ~ 3000 m. All samples are protogranular to porphyroclastic, granular lherzolites except for two mylonites at the end of the dive near the detachment fault footwall