Petrological, Geochemical and the Origin of the Cuobuzha Peridotite in the Western Yarlung Zangbo Suture Zone  

作　　者：FENG Guangying YANG Jingsui XIONG Fahui LIU Fei NIU Xiaolu LIAN Dongyang WANG Yunpeng ZHAO Yijue 

机构地区：[1]CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 10003 7, China [2]Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China [3]School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期10-11,共2页地质学报（英文版）

基　　金：financially supported by the National Nature Science Foundation of China (40930313, 40921001, 41303019);grants from Sinoprobe-05-02 of the Ministry of Science and Technology of China and the China Geological Survey (12120115027201)

摘　　要：Ophiolites are fragments of ancient oceanic lithosphere emplaced onto continental margins, accretionary prisms, or island arcs during plate collisions （Dilek and Fumes, 2011）. The well-preserved ophiolitic sequence provides important information on melt extraction, melting,Ophiolites are fragments of ancient oceanic lithosphere emplaced onto continental margins, accretionary prisms, or island arcs during plate collisions （Dilek and Fumes, 2011）. The well-preserved ophiolitic sequence provides important information on melt extraction, melting,

分 类 号：P588.125[天文地球—岩石学]