Neotectonics around the Ordos Block,North China  

作　　者：SHI Wei DONG Shuwen HU Jianmin 

机构地区：[1]SinoProbe Laboratory,Chinese Academy of Geological Science,Beijing 100086,China [2]School of Earth Sciences and Engineering,Nanjing University,Nanjing 211102,China [3]Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100086,China

出　　处：《Acta Geologica Sinica(English Edition)》2024年第S01期62-66,共5页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China(Grant No.41672203);China Geological Survey(CGS)(Grant Nos.DD20190018,DD20160060,1212011120099,1212011120100,1212011220259).

摘　　要：The Eurasian continent was subject to multiphase intensive intracontinental deformation in the Cenozoic(Fig.1A).However,its Cenozoic intra-continental deformation process and the driving force has long been disputed,which is only associated with the Indo-Asian collision(Molnar and Tapponnier,1975;Jolivet et al.,1990;Tapponnier et al.,2001;Yin,2010;Xu et al.,2013;Zhao et al.,2016),is caused by the Pacific-Asian collision(Cui,1997;Schellart and Lister,2005;Fan et al.,2019),or is connected with a combined effect of the Indo-Asian collision and the Pacific-Eurasia convergence(Ren et al.,2002;Li et al.,2013;Shi et al.,2015;Liu et al.,2019).

关 键 词：neotectonics faulted basin intracontinental deformation Indo-Asian collision Ordos Block Pacific-Asian collision North China 

分 类 号：P542[天文地球—构造地质学]