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 

作者机构：Institute of Geology and Mining China Nonferrous Metals (Guilin) Geology and Mining Co. Ltd Guilin 541004 CARMA State Key Laboratory of Continental Tectonics and Dynamics Institute of Geology Chinese Academy ofGeological Sciences Beijing 100037 Faculty of Earth Sciences China University of Geosciences Wuhan 430074 College of Resource and Environmental Engineering Guizhou University Guiyang 550025 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2015年第89卷第A02期

页      面：125-126页

核心收录：

学科分类：0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

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) 

主　　题：RESEARCH Ophiolites Suture zones (Structural geology) Geochemistry Mid-ocean ridges Petrogenesis Peridotite 

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,