Paleomagnetic,tectonic and geochronological constraints for Permian-Triassic oroclinal bending of the Mongolian collage  

作　　者：Karel Schulmann Jean Bernard Edel Ondrej Lexa Wenjiao Xiao D.Trebínová Richard Spikings Urs Schaltegger Arkadiusz Derkowski Marek Szczerba 

机构地区：[1]Centre for Lithospheric Research,Czech Geological Survey,Czech Republic [2]Institut Terre et Environnement de Strasbourg,Universitéde Strasbourg,France [3]Institute of Petrology and Structural Geology,Charles University,Czech Republic [4]Xinjiang Research Center for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,China [5]Earth and Environmental Sciences,Department of Earth Sciences,University of Geneva,Switzerland [6]Institute of Geological Sciences,Polish Academy of Sciences,Poland

出　　处：《National Science Review》2023年第2期4-6,共3页国家科学评论（英文版）

基　　金：financially supported by the GACR EXPRO Project 19-27682X to K.S.and O.L.;the National Natural Science Foundation of China(41888101)to W.X.;the International Partnership Program of Chinese Academy of Sciences(CAS)(132744KYSB20190039);IGCP 622(CAS)。

摘　　要：The Central Asian Orogenic Belt constitutes the Kazakhstan and Mongolian oroclinal collages located between the Tarim-North China collage(TNC)to the south and the Siberian craton to the north(Fig.1a)[1].While the oroclinal bending of the western Kazakhstan collage is widely accepted by the paleomagnetic and tectonic community,the oroclinal bending model of the eastern Mongolian collage is disputed[2,3].

关 键 词：TECTONIC Permian TRIASSIC 

分 类 号：P534[天文地球—古生物学与地层学] P548[天文地球—地质学] P318.44