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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)

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

Description

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

CollectionsANU Research Publications
Date published: 2013
Type: Journal article
URI: http://hdl.handle.net/1885/34554
Source: Lithos
DOI: 10.1016/j.lithos.2012.11.025

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