ZHANG Yong, REN Fenglou, GONG Shuyun, ZHANG Xianrong, LIN Manman, LIU Shanshan. CRETACEOUS STRESS FIELD OF THE MUPING-JIMO FAULT BELT AND ITS IMPLICATION FOR TECTONIC EVOLUTION[J]. Marine Geology & Quaternary Geology, 2013, 33(2): 79-85. DOI: 10.3724/SP.J.1140.2013.02079
Citation: ZHANG Yong, REN Fenglou, GONG Shuyun, ZHANG Xianrong, LIN Manman, LIU Shanshan. CRETACEOUS STRESS FIELD OF THE MUPING-JIMO FAULT BELT AND ITS IMPLICATION FOR TECTONIC EVOLUTION[J]. Marine Geology & Quaternary Geology, 2013, 33(2): 79-85. DOI: 10.3724/SP.J.1140.2013.02079
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CRETACEOUS STRESS FIELD OF THE MUPING-JIMO FAULT BELT AND ITS IMPLICATION FOR TECTONIC EVOLUTION

  • 1. Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao 266071, China;

  • 2. Qingdao Institute of Marine Geology, Qingdao 266071, China;

  • 3. Western District Research Center, Shengli Oil field, Dongying 257015, China;

  • 4. Shijiazhuang University of Economics, Shijiazhuang 050031, China;

  • 5. Geology Bureau of Shenzhen, Shenzhen 518023, China

More Information
  • Received Date: May 10, 2012
  • Revised Date: July 08, 2012
    Graphical Abstract
    • Abstract
  • Cretaceous is a key period for tectonic transformation in eastern China. Comparing to the Tan-Lu fault belt, the Jimo-Muping fault belt is another large-scale tectonic boundary in the east part of China. Many geologists have devoted to the studies of the structural characters and evolution history, especially those in Cretaceous, in the past decades. This time, we, based on the measured data, calculated the Cretaceous tectonic stress fields of the Muping-Jimo fault. The results indicate that the evolutionary history of the fault can be classified into five stages, i.e. 1) the Laiyang stage of Early Cretaceous dominated by NW-SE extension, under the control of the post-orogenic extension; 2) the Qingshan stage of Early Cretaceous dominated by W-E extension caused by a rifting process; 3) the NW-SE compression stage at the end of Early Cretaceous due to the oblique subduction of the Paleo-Pacific Plate under the East Asian continent; 4) the Wangshi stage of Late Cretaceous dominated by N-S extension, controlled by the Tethys system and the direction change of the subduction of the Paleo-Pacific Plate; 5) the stage of Late Paleocene dominated by NE-SW compression.
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    • References (19)
  • [1]
    陈柏林,王小凤,李中坚.苏胶地块北界应是五连-即墨-牟平断裂[J].地质力学学报,1996,2(3):23-24.

    [CHEN Bolin, WANG Xiaofeng, LI Zhongjian.The north boundary of Jiangsu-Shandong block is the Wulian-Jimo-Muping fracture[J].Journal of Geomechanics,1996,2(3):23-24.]
    [2]
    吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄[J].长春科技大学学报,1999,29(4):313-318.

    [WU Fuyuan, SUN Deyou.The Mesozoic magmatism and lithospheric thinning in eastern China[J].Journal of Changchun University of Science and Technology, 1999,29(4):313-318.]
    [3]
    肖文交, 周珧秀,杨振宇.大别-郯庐-苏鲁造山带复合旋转拼贴作用[J]. 地球科学进展,2000,15(2):147-153.

    [XIAO Wenjiao, ZHOU Yaoxiu, YANG Zhenyu.Multiple rotation and amalgamation progresses of Dabie-Tanlu-Sulu orogen[J]. Advance in Earth Sciences,2000,15(2):147-153.]
    [4]
    李三忠, 王金铎, 刘建忠,等. 鲁西地块中生代构造格局及其形成背景[J]. 地质学报,2005,79(4):487-497.

    [LI Sanzhong, WANG Jiduo, LIU Jianzhong,et al.Mesozic structure and its Tectonic setting in the western Shandong block[J].Acta Geologic Sinica, 2005,79(4):487-497.]
    [5]
    李三忠, 张国伟, 周立宏,等. 中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲[J]. 地学前缘, 2011,18(3):79-107.

    [LI Sanzhong, ZHANG Guowei, ZHOU Lihong,et al.The opposite Meso-Cenozoic intracontinental deformations under the superconvergence:Rifting and extension in the North China Craton and shortening and thrusting in the South China Craton[J].Earth Science Frontiers, 2011,18(3):79-107.]
    [6]
    LI Sanzhong, ZHAO Guochun, DAI Liming, et al. Cenozoic faulting of the Bohai Bay Basin and its bearings on the destruction of the eastern North China Craton[J]. Journal of Asian Earth Sciences, 2012b, 47:80-93.
    [7]
    LI Sanzhong, ZHAO Guochun, DAI Liming,et al. Mesozoic Basins in eastern China and their Bearings on the deconstruction of the North China Craton[J].Journal of Asian Earth Sciences,2012,47:64-79.
    [8]
    廖远涛. 胶莱盆地的盆地样式及构造演化[J].新疆石油地质,23(4),2002,345-347.

    [LIAO Yuantao.The pattern and tectonic evolution of Jiaolai Basin[J].Xinjiang Petroleum Geology,2002,345-347.]
    [9]
    吴智平, 李凌, 李伟,等.胶莱盆地莱阳期原型盆地的沉积格局及有利油气勘探区选择[J].大地构造与成矿学,2004,28(3):330-337.

    [WU Zhiping, LI Ling, LI Wei,et al. Sedimentary pattern of Prototype Basin in the deposition period of Laiyang Formation and the advantageous areas for oil and gas exploration of JiaoLai Basin[J]. Geotectonica et Metallogenia, 2004,28(3):330-337.]
    [10]
    乔秀夫,宋天锐,李海兵.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-34.

    [QIAO Xiufu, SONG Tianrui, LI Haibing. Seismic sequence in carbonate rocks by vibrational liquefIcation[J]. Acta Geologic Sinica,1994,68(1):16-34.]
    [11]
    乔秀夫,李海兵,高林志.华北地台震旦纪-早古生代地震节律[J].地学前缘, 1997, 4(3-4):155

    -160.[QIAO Xiufu, LI Haibing, GAO Linzhi. Sinian-Early Paleozoic seismic rhythms on the north china platform[J]. Earth Science Fronties,1997,4(3-4):155-160.]
    [12]
    吴福元,孙德有,张广良,等.论燕山运动的深部地球动力学本质[J].高校地质学报,2000,6(3):379-388.

    [WU Fuyuan, SUN Deyou, ZHANG Guangliang,et al.Deep geodynamics of Yanshan movement[J]. Geological Journal of China Universities,2000,6(3):379-388.]
    [13]
    ZHOU Xinhua,YANG Jinhui, ZHANG Lianchang.Metallogenesis of superlarge gold deposits in Jiaodong region and deep processes of subcontinental lithosphere beneath North China Craton in Mesozoic[J]. Science in China, 2002,46(Supp.):14-25.
    [14]
    翟明国,朱日祥,刘建明,等.华北东部中生代构造体制转折的关键时限[J].中国科学D辑,2003, 33(10):913-920.

    [ZHAI Mingguo, ZHU Rixiang, LIU Jianming,et al.Mesozoic tectonic regime inversion in eastern North China[J]. Science in China(Series D),2003, 33(10):913-920.]
    [15]
    XU Jiawei, ZHU Guang,TONG W X. Formation and evolution of the Tancheng-Lujiang wrench fault system:A major shear system to the northern of the Pacific Ocean[J]. Tectonophysics,1987,134:273-310.
    [16]
    朱光, 牛漫兰, 刘国生,等.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件[J]. 地质学报,2002,76(3):325-324.

    [ZHU Guang, NIU Manlan, LIU Guosheng, et al.Deformation, magmatism and sedimentary events during Early Cretaceous stike-sliping in the Tanlu Fault[J]. Acta Geologic Sinica,2002,76(3):325-324.]
    [17]
    朱光, 刘国生, W J Dunlap,等.郯庐断裂带同造山走滑运动的40Ar/39Ar年代学证据科学通报,2004,49(2):190-198.

    [ZHU Guang, LIU Guosheng, W J Dunlap,et al.40Ar/39Ar geochronological constraints on syn-orogenic strike-slip movement of the Tan-Lu fault zone[J]. Chinese Science Bulletin,2004,49(2):190-198.]
    [18]
    张宏远, 侯泉林, 曹代勇.胶东东部中生代走滑逆冲构造带的构造年代学制约[J].中国科学D辑,2006,36(6):497-506.

    [ZHANG Hongyuan, HOU Qianlin, CAO Daiyong.Jiaodong Mesozoic strike slip thrust belt tectonic geochronology[J]. Science in China(Series D),2006,36(6):497-506.]
    [19]
    张宏远, 侯泉林, 曹代勇.胶东东部中生代逆冲推覆构造研究[J]. 中国科学D辑,2006,36(7):593-600.

    [ZHANG Hongyuan, HOU Quanlin, CAO Daiyong. The study of Mesozoic thrust nappe structure in eastern Jiaodong[J]. Science in China (Series D),2006,36(7):593-600.]
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