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MESOZOIC DEXTRAL STRIKE-SLIP STRUCTURAL SYSTEM IN MIDDLE SEGMENT OF INTRAPLATE YANSHAN OROGENIC BELT, NORTHERN CHINA

Zhang Changhou, Song Honglin, Wang Genhou, Yan Danping, Sun Weihua (Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing100083, China)  
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described. The dextral strike-slip fault system is composed of east-west oriented master faults - Gubeikou-Pingquan fault zone and Miyun-Xifengkou fault zone, with the structures between them such as the northeast strike contractional faults and associate folds, northwest oriented extensional faults and dykes as well. The master east-west faults are characterized by subordinate right lateral overstep en echlon faults. While the northwest striking extensional faults and dykes are comparable to "T fractures" expected by Riedel model. The northeast oriented contractional faults and related folds, meanwhile, are the counterparts of compressive structures in Riedel model. The combination of the master faults with the associate northeast fault and folds makes a strike-slip duplex structure. The strike-slip faults formed between later Jurassic and Early Cretaceous. Giving the temporal and spatial relationship among the east-west trending dextral strike-slip fault system and the southeast-ward thrust faulting in the eastern part and the northwestward thrust fault system in the western segment of the Yanshan belt, a unified tectonic model - dextral slip system has been established. This model leads to a renewed interpretation of the tectonic framework and evolution of the Mesozoic-Cenozoic intraplate Yanshan orogenic belt. In this model, the two thrust systems with opposite movement directions in western Liaoning and northwestern Hebei provinces are considered as the result of the compressions in the front of dextral strike-slip plates northeast and southwest of the master fault, respectively. It is reasonable to infer that the tectonic framework of the late Mesozoic intraplate Yanshan orogen is dominated by east-west dextral strike-slip faulting and related deformation. Furthermore, the intraplate Yanshan orogenic belt might be another "extrusion tectonic belt" or "escape tectonics" during the Jura-Cretaceous time in the frame of northeastern Asia. However, a synchronous sinistral strike-slip fault zone north to this belt is needed to prove this interpretation.
【Fund】: 国家自然科学基金 (No .4970 2 0 34 ;;No .49772 14 8) ;; 中国地质调查局 1∶2 5万青龙县幅 ( 2 0 0 0 130 0 0 0 5 14 1)地质调查项目
【CateGory Index】: P542
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2 ZHANG YuTao,ZHANG LianChang,YING JiFeng,ZHOU XinHua,WANG Fei,HOU QuanLin and LIU Qing 1.Key laboratory of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China 2.State key laboratory of lithospheric evolution,Institute of Geology and Geophysics,CAS,Beijing 100029,China 3.Graduate university of Chinese Academy of Sciences,Beijing 100039,China;Geochemistry and source characteristics of early Cretaceous volcanic rocks in Tahe,north Da Hinggan Mountain.[A];[C];2008
3 Li Zhong~1 Dong Renguo~2 Zheng Jianping~3 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029 2 Shandong Survey Institute of Geology and Mineral Resources,Jinan 250014,Shandong 3 China University of Geosciences,Wuhan 420073,Hubei;Mesozoic volcanic-sedimentary configurations in north and south margins of the eastern North China Craton:Implications for tectonic transition mechanism[A];[C];2008
4 ZHAI MingGuo Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2008-05-29收稿,2008-09-10改回.;Lower crust and lithospheric mantle beneath the North China Craton before the Mesozoic lithospheric disruption.[A];[C];2009
5 CHEN ZhiGuang,ZHANG LianChang,WU HuaYing,WAN Bo and ZENG QingDong 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100039,China;Geochemistry study and tectonic background of A style host granite in Nianzigou molybdenum deposit in Xilamulun molybdenum metallogenic belt,Inner Mongolia.[A];[C];2009
6 WU HuaYing,ZHANG LianChang,ZHOU XinHua and CHEN ZhiGuang 1.Key laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.State key laboratory of litho spheric evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 3.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Geochronology and Geochemical characteristics of Late Mesozoic andesites in the Central Da-Hinggan Mountains,and its genesis.[A];[C];2009
7 LONG Fan~1,HAN Tiancheng~1,YU Dehao~(1,2) (1.Engineering Research Institute,Shenyang Military Area Command,Shenyang, 110162,China;2.65056 Troops,Tieling,112000,China);The Application of Remote Sensing to the Water Reconnaissance in the West Areas of Liaoning Province[A];[C];2010
8 ZHAI Mingguo,ZHU Rixiang,LIU Jianming,MENG QingFen,HOU Quanlin, HU Shengbiao,LIU Wei,LI Zhong,ZHANG Hongfu & ZHANG Huafeng Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Time range of Mesozoic tectonic regime inversion in eastern North China Block[A];[C];2004
9 Tianyu Zheng~(a,*),Ling Chen~a,Liang Zhao~a,Rixiang Zhu~b a Seismological Laboratory(SKL-LE),Institute of Geology and Geophysics,Chinese Academy of Sciences,China b Palaeomagnetism and Geochronology Laboratory(SKL-LE),Institute of Geology and Geophysics, Chinese Academy of Sciences,China;Crustal structure across the Yanshan belt at the northern margin of the North China Craton[A];[C];2008
10 Z.LI~1,Y.LI~2,J.-P.ZHENG~3 & D.HAN~1 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China 2 Shengli Oil field,SINOPEC,Dongying 256504,China 3 China University of Geosciences,Wuhan 420073,China;Late Mesozoic tectonic transition of the eastern North China Craton:evidence from basin-fill records[A];[C];2008
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Chinese Journal Full-text Database 10 Hits
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4 Shan Wenlang Fu Zhaoren (Wuhan College of Geology, Wuhan 430074);A PRELIMINARY ANALYSIS OF THE HORIZONTAL LAMINAR SHEAR-FLOW STRUCTURE IN THE WEST-HILL,BEIJING[J];;1987-02
5 Fei Qi ( Wuhan College of Geology, Wuhan 430074);A PRELIMINAEY RESEARCH INTO THE PLATE COLLISION,ROTATION AND DIVERGENCE PATTERN OF CHINA AND ITS PERIPHERY SINCE MESOZOIC[J];;1987-05
6 Ye Junlin Zhu Zhicheng Xiang Shuyuan. Zhang Gouxin ( Wuhan college of Geology, Wuhan 430074 );ON STYLES AND MECHANISM OF THRUST ON THE SOUTH MARGIN OF INNER MONGOLIA AXIS[J];;1987-05
7 Ye Junlin Xiang Shuyuan ( China University of Geosciences, Wuhan 430074 );THE CHARACTERISTICS AND FORMATION MECHANISM OF THRUST-NAPPE STRUCTURE IN MAGMATIC BODY AREA IN CHICHENG, HEBEI PROVINCE[J];;1989-01
8 LIU YUAN-LUNG WANG QIAN-SIIEN ZHAO JIAN-HUA(Institute of Geophysics, Academia Sinica);A PRELIMINARY STUDY BASED ON GRAVITY DATA OF THE CRUSTAL STRUCTURE OF THE PEKING-TIENTSIN AREA AND ITS NEIGHBORING REGIONS[J];Chinese Journal of Sinica;1978-01
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10 Li Zhitong Zhao Chunjing (Shenyang Institute of Geology and Mineral Resources);INDOSINIAN MOVEMENT IN NORTHEASTERN CHINA[J];Chinese Journal of Geology;1985-03
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