New timing of the Indosinian intracontinental deformation from the Triassic growth strata in the Kuqa Depression,Southern Tianshan,China  

作　　者：Xiang Qin Xuan-hua Chen Zhao-gang Shao Yi-ping Zhang Yong-chao Wang 

机构地区：[1]Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China

出　　处：《China Geology》2022年第4期771-773,共3页中国地质（英文）

基　　金：supported by the National Key Research and Development Project(2018YFC0603700);projects of the China Geological Survey(DD20160083,DD20190011).

摘　　要：1.Objectives In the Indosinian duration,series of Gondwana-related plates pieced together and formed the geological sketch of China for the first time,i.e.the Yangtze,Sino Korean,Tarim plates,and other sub-plates that had been isolated for a long time.Subduction and collision among the Tarim,Qaidam,and Qiangtang blocks in Triassic,as well as the closure of the Paleo-Tethys Ocean,reactivated Late Paleozoic suture zones in the Tianshan orogen region(Hendrix MS et al.,1992).

关 键 词：TIANSHAN TRIASSIC STRATA 

分 类 号：P548[天文地球—构造地质学] P534.51[天文地球—地质学]