Neotectonics around the Ordos Block,North ChinaOACSTPCD
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).
SHI Wei;DONG Shuwen;HU Jianmin
SinoProbe Laboratory,Chinese Academy of Geological Science,Beijing 100086,ChinaSinoProbe Laboratory,Chinese Academy of Geological Science,Beijing 100086,China School of Earth Sciences and Engineering,Nanjing University,Nanjing 211102,ChinaInstitute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100086,China
地质学
neotectonics,faulted basin,intracontinental deformation,Indo-Asian collision,Ordos BlockPacific-Asian collision,North China
《Acta Geologica Sinica(English Edition)》 2024 (S01)
P.62-66,5
supported by the National Natural Science Foundation of China(Grant No.41672203)China Geological Survey(CGS)(Grant Nos.DD20190018,DD20160060,1212011120099,1212011120100,1212011220259).
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