Mantle source and magma oxygen fugacity of Permian Ni--Cu sulfide-bearing mafic-ultramafic intrusions in the Inner Mongolia, North China: Controls on the sulfide saturation of magmas in the Andean-style continental convergent margins-Reference-Cited by-同舟云学术

Mantle source and magma oxygen fugacity of Permian Ni--Cu sulfide-bearing mafic-ultramafic intrusions in the Inner Mongolia, North China: Controls on the sulfide saturation of magmas in the Andean-style continental convergent margins

Published:2021-06 Issue: Volume:390-391 Page:106105
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Cao Yonghua,Wang Christina Yan,Wei Bo,Bao Hongtian

Funder

Guangzhou Institute of Geochemistry

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference80 articles.

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4. Variation in sub-arc mantle oxygen fugacity during partial melting recorded in refractory peridotite xenoliths from the West Bismarck Arc;Bénard;Chem. Geol.,2018

5. Temporal evolution of mantle wedge oxygen fugacity during subduction initiation;Brounce;Geology,2015

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