Two stages of crust-mantle interaction during oceanic subduction to continental collision: Insights from mafic-ultramafic complexes in the North Qaidam orogen

Subducted sedimentary rocks contribute to different reservoirs in the mantle, which results in crust-mantle interaction; however, the metasomatic processes involved in this sedimentary contribution to the mantle still remain poorly understood. Chromite is a robust mineral and together with its inclu...

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Bibliographic Details
Published inGondwana research Vol. 89; pp. 247 - 264
Main Authors Cai, Pengjie, Chen, Xin, Majka, Jarosław, Klonowska, Iwona, Jeanneret, Pauline, Xu, Rongke, Zheng, Youye
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.01.2021
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