Geogenesis and Characteristics of the Western Part of the Yarlung Zangbo Ophiolites, Tibet  

作　　者：LIU Fei YANG Jingsui LIAN Dongyang ZHAO Hui ZHANG Lan NIU Xiaolu FENGGuangying ZHANG Li HUANG Jian 

机构地区：[1]CARMA, State Key Laboratory of Continental Tectonic and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037, China [2]Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China [3]Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083, China

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期52-55,共4页地质学报（英文版）

基　　金：funded by grants from 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 ophiolites that crop out discontinuously for more than 2000 km along the Yarlung-Zangbo suture zone （YZSZ, also called the Indus-Tsangpo suture） in southern Tibet are the remnants of the Neotethyan oceanic lithosphere,The ophiolites that crop out discontinuously for more than 2000 km along the Yarlung-Zangbo suture zone （YZSZ, also called the Indus-Tsangpo suture） in southern Tibet are the remnants of the Neotethyan oceanic lithosphere,

分 类 号：P588[天文地球—岩石学]