Early Paleozoic Mafic-Ultramafic Rocks in the East Kunlun: Trace Subduction of Proto-Tethys  

作　　者：MENG Fancong CUI Meihui REN Yufeng Paul T.ROBINSON 

机构地区：[1]Institute of Geology, Chinese Academy of Geological Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2016年第S1期231-233,共3页地质学报（英文版）

基　　金：supported by National Natural Science Foundation of China(41072026,41272052);the China Geological Survey project(1212010918003,1212011120158)

摘　　要：The East Kunlun located in the northern margin of the Qinghai-Xizang(Tibet)Plateau,is a composite orogenic belt which has underwent multi-stages tectonic evolution(e.g.Wang and Chen,1987;Jiang et al.,1992;Yang et al.,1996,2009).The East Kunlun orogenic belt(EKOB)is bounded by Altyn Tagh Fault in the west and Wenquan Fault in the east,bounded by the south margin of Qaidam

关 键 词：Trace Subduction of Proto-Tethys Early Paleozoic Mafic-Ultramafic Rocks in the East Kunlun PB PPM 

分 类 号：P588[天文地球—岩石学]