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《Chinese Journal of Geophysics》 2007-01
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Aeromagnetic anomaly analysis of Ordos and adjacent regions and its tectonic implications

WANG Tao~1,XU Ming-Jie~1,WANG Liang-Shu~1,LIU Shao-Wen~2,HU Xu-Zhi~11 Department of Earth Sciences,Nanjing University,Nanjing 210093,China2 School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,China  
Affiliated to the North China Craton(NCC),the Ordos massif contacts with the Qinling-Qilian orogenic belt to the south,with complicated geological features around as a result of episodic tectonics.By applying the upward continuation,vertical derivation of different orders,and a new method for delineating magnetic boundaries to the aeromagnetic data,as well as taking into account the earthquake data,here we present the characteristics of aeromagnetic anomalies of field sources at different depths and their tectonic implications.Our results show that the basement of the Ordos is rigid on the whole but is still heterogeneous.The east of the Ordos massif in NCC is a relatively weak zone with approximately NS trending suffered from subsequent tectonic alternation.The ductile lower crustal material flows along two weak zones of the Qinling and Qilian orogenic belt coevally with the thickening and shortening of the crust in Qinghai-Tibet Plateau,as well as the anticlockwise rotation of the Ordos massif due to the intensive compressional stress in NE direction derived from the India-Eurasia collision.The diverse tectonic features mentioned above in and along the margins of the Ordos massif represent the tectonic responses of the crustal blocks of different rigidity to the boundary forces,that resulted in prominently different geological features.The tectonic deformation in and around the Ordos massif is characterized by inheritance and superimposition.
【Fund】: 国家自然科学基金项目(40474017);; 国家基础科学人才培养基金项目资助
【CateGory Index】: P631.222
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4 LU LiNa,FAN HongRui~(**),HU FangFang,YANG KuiFeng and LAN TingGuang Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Emplacement depth of the Guojialing granodiorites from the northwestern Jiaodong Peninsula,eastern China:Evidences from hornblende thermobarometry and fluid inclusions[A];[C];2012
5 GUO Zhi-hua,ZHANG Bao-lin~*,QI Min,JIA Wen-cheng, SHEN Xiao-li,HUANG Xue-fei (Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);The application of high precision ground magnetic prospecting for geological mapping in the 13451 mining area in Mongolia[A];[C];2012
6 TENG Ji-Wen~1,WANG Fu-Yun~2,ZHAO Wen-Zhi~3,ZHANG Yong-Qian~1,ZHANG Xian-Kang~2, YAN Ya-Fen~1,ZHAO Jin-Ren~2,LI Ming~3,YANG Hui~1,ZHANG Hong-Shuang~1,RUAN Xiao-Min~1 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Geophysical Exploration Center,China Earthquake Administration,Zhengzhou 450002,China 3 SINOPEC Research Institute of Potroloum Exploration and Development,Beijing 100083,China;Velocity structure of layered block and deep dynamic process in the lithosphere beneath the Yinshan orogenic belt and Ordos Basin[A];[C];2011
7 WANG Qian-shen~1,TENG Ji-wen~1,AN Yu-lin~2,ZHANG Yong-qian~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.China University of Geosciences,Beijing 100083,China);Gravity field and deep crustal structures of the Yinshan orogen and the northern Ordos basin[A];[C];2011
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10 WEI Zi-Gen,CHEN Ling State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China;Regional differences in crustal structure beneath northeastern China and northern North China Craton:constraints from crustal thickness and V_p/V_s ratio[A];[C];2013
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