The recycling of chromitites in ophiolites from southwestern North America

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The recycling of chromitites in ophiolites from southwestern North America

© 2017 Elsevier B.V. Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite, Baja California Sur State, Mexico. These are high-Cr chromitites [Cr# (Cr/Cr + Al atomic ratio = 0.61–0.69)] that contain a range of minor- and trace-elements and show whole-rock enrich...

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Bibliographic Details
Main Authors:	González-Jiménez, J., Camprubí, A., Colás, V., Griffin, W., Proenza, J., O'Reilly, S., Centeno-García, E., García-Casco, A., Belousova, E., Talavera, Cristina, Farré-de-Pablo, J., Satsukawa, T.
Format:	Journal Article
Published:	Elsevier BV 2017
Online Access:	http://hdl.handle.net/20.500.11937/58948

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