Skip navigation
Skip navigation
The system will be down for maintenance between 8:00 and 8:15am on Wednesday 12, December 2018

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.


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
Source: Lithos
DOI: 10.1016/j.lithos.2012.11.025


File Description SizeFormat Image
01_Marchesi_Element_mobility_from_seafloor_2013.pdf2.63 MBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  27 November 2018/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator