A shallow origin for diamonds in ophiolitic chromitites

Author:

Farré-de-Pablo Júlia1,Proenza Joaquín A.1,González-Jiménez José María2,Garcia-Casco Antonio23,Colás Vanessa4,Roqué-Rossell Josep1,Camprubí Antoni4,Sánchez-Navas Antonio23

Affiliation:

1. Department of Mineralogy, Petrology and Applied Geology, University of Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain

2. Department of Mineralogy and Petrology, Faculty of Sciences, University of Granada, Avenida Fuentenueva s/n, 18002 Granada, Spain

3. Andalusian Earth Science Institute (IACT), Spanish Research Council (CSIC)–University of Granada, Avenida de las Palmeras, 4, 18100 Armilla, Granada, Spain

4. Institute of Geology, National Autonomous University of Mexico, Ciudad Universitaria, 04510 Ciudad de México, Mexico

Publisher

Geological Society of America

Subject

Geology

Reference22 articles.

1. Characterization of amorphous and nanocrystalline carbon films;Chu;Materials Chemistry and Physics,2006

2. The role of silica in the hydrous metamorphism of chromite;Colás;Ore Geology Reviews,2017

3. A reappraisal of the metamorphic history of the Tehuitzingo chromitite, Puebla State, Mexico;Colás;International Geology Review,2018

4. Diamond formation by carbon saturation in C-O-H fluids during cold subduction of oceanic lithosphere;Frezzotti;Geochimica et Cosmochimica Acta,2014

5. A high-pressure folded klippe at Tehuitzingo on the western margin of an extrusion zone, Acatlán Complex, southern México;Galaz;Gondwana Research,2013

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