Constraints of late Cambrian mafic rocks from the Qushi'ang ophiolite on a back-arc system in a continental margin, East Kunlun Orogen, Western China

Ruibao Li,Xianzhi Pei,Bo Wei,Zuochen Li,Lei Pei, Youxin Chen,Chengjun Liu, Guochao Cheng,Meng Wang,Keng Feng

Journal of Asian Earth Sciences（2019）

引用 30|浏览26

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摘要

•498–505 Ma ophiolites occurred in the East Kunlun orogen.•Mafic rocks are derived from melting of a mantle wedge.•The ophiolite represents a relict of nascent back-arc basin.

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关键词

Supra-subduction zone,Backarc basin,Ophiolite,East Kunlun,Proto-Tethys,Cambrian

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