Early Permian Qiangtang Mantle Plume, Northern Tibet, China: Evidence from Geochemistry, Geochronology and Geological Responses  

作　　者：ZHOU Xiaoyao JIN Xin ZHANG Yuxiu 

机构地区：[1]Key Laboratory of Computational Geodynamics, Chinese Academy of Sciences [2]Asian Tectonics Research Group, College of Earth Science, University of Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期138-140,共3页地质学报（英文版）

基　　金：supported by the Natural Science Foundation of China (41472209 and 40802048);the Chinese Academy of Sciences (Y129012EA2 and 118900EA12);the President Fund for Science and Education Fusion of UCAS (Y552011Y00)

摘　　要：Late Paleozoic igneous rocks are extensively developed in Qiangtang terrene,including west Qiangtang(WQT),east Qiangtang(EQT)and the central Qiangtang(CQT)metamorphic belt.The igneous rocks distributed in WQT

关 键 词：Zhang OIB Geochronology and Geological Responses China Early Permian Qiangtang Mantle Plume Evidence from Geochemistry 

分 类 号：P542.5[天文地球—构造地质学] P534.46[天文地球—地质学]