Multi-scale development of a stratiform chromite ore body at the base of the dunitic mantle-crust transition zone (Maqsad diapir, Oman ophiolite): The role of repeated melt and fluid influxes-Reference-Cited by-同舟云学术

Multi-scale development of a stratiform chromite ore body at the base of the dunitic mantle-crust transition zone (Maqsad diapir, Oman ophiolite): The role of repeated melt and fluid influxes

Published:2019-12 Issue: Volume:350-351 Page:105235
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Rospabé Mathieu,Ceuleneer Georges,Granier Nicolas,Arai Shoji,Borisova Anastassia Y.

Funder

Centre National de la Recherche Scientifique

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference87 articles.

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3. Synmagmatic normal faulting in the lower oceanic crust: evidence from the Oman ophiolite;Abily;Geology,2011

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

5. Tectonic setting for the genesis of oceanic plagiogranites: evidence from a paleo-spreading structure in the Oman ophiolite;Amri;Earth Planet. Sci. Lett.,1996

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