Gongzhucuo Massif: An Ever Slightly Depleted Peridotite in the Western Yarlung Zangbo Ophiolitic Belt of Southern Tibet  

作　　者：ZHANG Li YANG Jingsui LIANDongyang LIU Fei ZHAO Hui HUANG Jian YANG Yan 

机构地区：[1]School of Earth Sciences and Resources, China University of Geoscienees, Beo'ing 100083, China [2]CARMA, State Key Laboratory forContinental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China [3]Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期117-119,共3页地质学报（英文版）

基　　金：the Ministry of Science and Technology of China (2014DFR21270);China Geological Survey (12120115026801, 12120115027201, 201511022);the Fund from the State Key Laboratory of Continental Tectonics and Dynamics (Z1301-a20)

摘　　要：The Gongzhucuo ophiolite, located near Lake Gongzhu in SW Tibet, occurs in the southern ophiolite sub-belt along the western YarlungZangbo suture zone. It is is mainly composed of harzburgitic and lherzolitic upper mantle oeridotites,The Gongzhucuo ophiolite, located near Lake Gongzhu in SW Tibet, occurs in the southern ophiolite sub-belt along the western YarlungZangbo suture zone. It is is mainly composed of harzburgitic and lherzolitic upper mantle oeridotites,

分 类 号：P588.125[天文地球—岩石学]