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

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

Chromitite bodies hosted in peridotites typical of suboceanic mantle (s.l. ophiolitic) are found in the northern and central part of the Loma Caribe peridotite, in the Cordillera Central of the Dominican Republic. These chromitites are massive pods of small size (less than a few meters across) and v...

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Bibliographic Details
Main Authors:	Júlia Farré-de-Pablo, Joaquín A. Proenza, José María González-Jiménez, Thomas Aiglsperger, Antonio Garcia-Casco, Javier Escuder-Viruete, Vanessa Colás, Francisco Longo
Format:	Article
Language:	English
Published:	Elsevier 2020-11-01
Series:	Geoscience Frontiers
Subjects:	Chromitite Ophiolite Plume Mantle Back-arc basin Dominican Republic
Online Access:	http://www.sciencedirect.com/science/article/pii/S1674987120301237

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