Neotectonics around the Ordos Block,North China

作     者：SHI Wei DONG Shuwen HU Jianmin SHI Wei;DONG Shuwen;HU Jianmin

作者机构：SinoProbe LaboratoryChinese Academy of Geological ScienceBeijing 100086China School of Earth Sciences and EngineeringNanjing UniversityNanjing 211102China Institute of GeomechanicsChinese Academy of Geological SciencesBeijing 100086China 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2024年第98卷第S01期

页      面：62-66页

核心收录：

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 

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) 

主　　题：neotectonics,faulted basin,intracontinental deformation,Indo-Asian collision,Ordos Block Pacific-Asian collision,North China 

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).