No evidence of progressive serpentinization at slow-slip oceanic transform faults: Geophysical constraints from the Vema Transform, Central Atlantic


Marco Cuffaro1, Marco Ligi2 and Enrico Bonatti2,3, (1)IGAG-CNR, Rome, Italy, (2)CNR Institute for Marine Science, Bologna, Italy, (3)Lamont Doherty Earth Observatory, Columbia University, Palisades, United States
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