Petrogenesis of Peridotites from the Purang Ophiolite in Western Part of Yarlung-Zangbo Suture Zone, Southern Tibet  

作　　者：ZHOU Wenda YANG Jingsui ZHAO Junhong MA Changqian XIONG Fahui XU Xiangzhen CHEN Yanhong TIAN Yazhou 

机构地区：[1]Institute of Geology and Mining, China Nonferrous Metals (Guilin) Geology and Mining Co., Ltd, Guilin 541004 [2]CARMA, State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy ofGeological Sciences, Beijing 100037 [3]Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074 [4]College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期125-126,共2页地质学报（英文版）

基　　金：supported 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：Peridotites are an important part of ophiolites： they not only record plate tectonic settings and events, but also offer help to interpret the composition of the mantle and the effect of the deep mantle. The Yarlung-Zangbo suture zone extends more than 2000 km along southern Tibet,Peridotites are an important part of ophiolites： they not only record plate tectonic settings and events, but also offer help to interpret the composition of the mantle and the effect of the deep mantle. The Yarlung-Zangbo suture zone extends more than 2000 km along southern Tibet,

分 类 号：P588.125[天文地球—岩石学]