High-P metamorphism of rodingites during serpentinite dehydration (Cerro del Almirez, Southern Spain): Implications for the redox state in subduction zones-Reference-Cited by-同舟云学术

High-P metamorphism of rodingites during serpentinite dehydration (Cerro del Almirez, Southern Spain): Implications for the redox state in subduction zones

Published:2018-08-30 Issue:9 Volume:36 Page:1141-1173
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Laborda-López Casto¹^ORCID,López-Sánchez-Vizcaíno Vicente¹,Marchesi Claudio²³,Gómez-Pugnaire María T.²³,Garrido Carlos J.²,Jabaloy-Sánchez Antonio⁴,Padrón-Navarta José A.⁵,Hidas Károly²

Affiliation:

1. Departamento de Geología (Unidad Asociada al IACT-CSIC); Universidad de Jaén; Linares Spain

2. Instituto Andaluz de Ciencias de la Tierra; CSIC-Universidad de Granada; Armilla (Granada) Spain

3. Departamento de Mineralogía y Petrología; Universidad de Granada; Granada Spain

4. Departamento de Geodinámica; Universidad de Granada; Granada Spain

5. Géosciences Montpellier; UMR 5243; CNRS-Université de Montpellier; Montpellier France

Funder

Ministerio de Economía y Competitividad

Junta de Andalucía

Ramón y Cajal

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12440/fullpdf

Reference118 articles.

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4. The crystal chemistry of birefringent natural uvarovites. Part IV. OH defect incorporation mechanisms in non-cubic garnets derived from polarized IR spectroscopy;Andrut;European Journal of Mineralogy,2002

5. Rodingite occurrences in some Archaean ultramafic complexes in the Barberton Mountain Land, South-Africa;Anhaeusser;Precambrian Research,1979

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