Ophiolite hosted chromitite formed by supra-subduction zone peridotite –plume interaction

Author:

Farré-de-Pablo Júlia,Proenza Joaquín A.,González-Jiménez José María,Aiglsperger Thomas,Garcia-Casco Antonio,Escuder-Viruete Javier,Colás Vanessa,Longo Francisco

Funder

Fondo Europeo de Desarrollo Regional (FEDER) Funds

Ministerio de Economía y Competitividad

Ministerio de Ciencia, Innovación y Universidades

Ramón y Cajal Fellowship

Mexican research programs Ciencia Básica

Consejo Nacional de Ciencia y Tecnología

University of Barcelona

University of Granada

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference153 articles.

1. Unexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonic implications;Ahmed;Contrib. Mineral. Petrol.,2002

2. Platinum group minerals (PGM) in the Falcondo Ni-laterite deposit, loma Caribe peridotite (Dominican Republic);Aiglsperger;Miner. Deposita,2015

3. Thermochemical behavior of Pt, Ir, Rh and Ru vs. fO2 and fS2 in a basaltic melt. Implications for the differentiation and precipitation of these elements;Amossé;Mineral. Petrol.,2000

4. Experimental observation on noble metal nanonuggets and Fe-Ti oxides, and the transport of platinum group elements in silicate melts;Anenburg;Geochem. Cosmochim. Acta,2016

5. Conversion of low-pressure chromitites to ultrahigh-pressure chromitites by deep recycling: a good inference;Arai;Earth Planet Sci. Lett.,2013

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