Oxygen fugacity range of subducting crust inferred from fractionation of trace elements during fluid-present slab melting in the presence of anhydrite versus sulfide-Reference-Cited by-同舟云学术

Oxygen fugacity range of subducting crust inferred from fractionation of trace elements during fluid-present slab melting in the presence of anhydrite versus sulfide

Published:2022-05 Issue: Volume:325 Page:214-231
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Chowdhury Proteek,Dasgupta Rajdeep,Phelps Patrick R.,Costin Gelu,Lee Cin-Ty A.

Funder

National Science Foundation

Geological Society of America

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference75 articles.

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