Fig. 6
From: The Atlantis Bank Gabbro Massif, Southwest Indian Ridge
British Geological Survey diamond drill cores from the Atlantis Bank wave-cut platform documenting the presence of: 12-1 - carbonate veined serpentine ophicalcite in the eroded fault damage zone (JCR31 BGS 12-1 0–32 cm); -13-1 bioclastic carbonate-cemented weathered pillow basalt breccia cemented clastic breccia hanging wall debris (JCR31 BGS 13-1 29–64 cm) deposited on the fault surface; 14-1 bioclastic limestone from the fringing fossil beach around the platform (JCR31 BGS 14-1 0–36 cm)