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Element mobility from seafloor serpentinization to high-pressure dehydration of antigorite in subducted serpentinite: Insights from the Cerro del Almirez ultramafic massif (southern Spain)

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Authors

Marchesi, C
Garrido, Carlos J
Padron-Navarta, Jose
Lopez Sanchez-Vizcaino, Vicente
Gómez-Pugnaire, M.T.

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Elsevier

Abstract

The Cerro del Almirez ultramafic massif is composed of antigorite serpentinite and chlorite harzburgite separated by a narrow transitional zone that marks the front of prograde serpentinite-dehydration at high pressure in a paleo-subduction setting. Conce

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Lithos

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Restricted until

2037-12-31