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Mantle peridotites from an exposed lithospheric section (Vema Lithospheric Section, VLS), generated during ~26Ma at a ~80km long Mid Atlantic Ridge segment (11° N), have been sampled and studied to understand the evolution of the serpentinization process. The VLS was uplifted due to a 10Ma transtensional event along the Vema transform. Before the uplift residual mantle rocks were lying beneath a 0...
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