Element mobility from seafloor serpentinization to high-pressure dehydration of antigorite in subducted serpentinite: Insights from the Cerro del Almirez ultramafic massif (southern Spain)
-
Altmetric Citations
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
| Collections | ANU 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 |
Download
| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Marchesi_Element_mobility_from_seafloor_2013.pdf | 2.63 MB | Adobe PDF | Request a copy |
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.
Updated: 17 November 2022/ Responsible Officer: University Librarian/ Page Contact: Library Systems & Web Coordinator
+61 2 6125 5111
The Australian National University, Canberra
CRICOS Provider : 00120C
ABN : 52 234 063 906
