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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: The Atlantis Bank Gabbro Massif, Southwest Indian Ridge

Fig. 6

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)

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