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The structural and tectonic relationships of the major fault systems of the Tan-Lu fault zone,with a focus on the segments within the North China region

The structural and tectonic relationships of the major fault...

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中国科学院地质与地球物理研究所2015年度（第15届）学术年会

作者： Jiaodong Zhang Tianyao Hao Shuwen Dong Xuanhua Chen Jianjun Cui Xiaoyong Yang Chengzhai Liu Tiejun Li Ya Xu Song Huang Fenglou Re Key Laboratory of Petroleum Resources Research Institute of Geology and GeophysicsChinese Academy of Sciences Chinese Academy of Geological Sciences School of Earth and Space Sciences University of Science and Technology of China The Shengli Oil Company

The Jiashan-Lujiang,Yishu and Bohai segments have been the most tectonically active parts of the Tan-Lu fault system since the *** analysis of faulting processes in the Tan-Lu system is highly dependent on the relationships among the three *** we divide the Tan-Lu system into three styles of faulting;strike-slip faulting,regional extensional faulting and listric normal faulting on the basis of EMAP data,seismic profiles and geological *** suggest that:(1) the strike-slip faults,which formed in the Late Jurassic,include mainly the Jiashan-Lujiang fault,the deep parts of the Chihe-Taihu Fault and the Guhe-Sanbing fault;these three faults have had the most dramatic effect on the JiashanLujiang *** strike-slip style of faulting produced a huge positive-flower structure that extends between the deep section of the Chihe-Taihu fault and the Guhe-Sanbing fault,and overlaps with the position of the Zhangbaling ductile shear zone;(2) the regional extensional style of faulting,whose characteristics are reflected best in the Yishu fault zone,is composed of the Changyi-Dadian,Anqiu-Quxian,Yishui-Yangtou and Tangwu-Gegou faults,all of which were active during the Early *** extension-dominated faults extend southwards to the Jiashan and Hefei Basins and die out in front of the Dabie Mountains;to the north,the faults penetrate the deeper parts of the Weibei depression where they controlled Cretaceous deposition in "graben-horst-graben" structures;(3) the listric normal faults,which were initiated in the Paleogene,generally occur around the Bohai Bay Basin,and include a series of NE-trending faults in the Weibei depression,such as the Tandong and Tanxi *** listric faults differ from the regional extensional faults in their localized occurrence and association with basin *** study indicates that these three styles of faulting varied not only in timing and mechanical properties but developed at different levels at dif

关键词： Tan-Lu fault zone Fault systems tectonic relationships Meso-Cenozoic Space-time framework

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