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    Volume 49 Issue 6
    Jun.  2024
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    Article Navigation >  Earth Science  > 2024  >  49(6): 2071-2084
    Li Wei, Li Jia, Wu Wanqiu, Zhang Tongjie, Chen Xingpeng, Meng Meifang, Cao Mingyue, Zhang Qiao, 2024. Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone. Earth Science, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480
    Citation: Li Wei, Li Jia, Wu Wanqiu, Zhang Tongjie, Chen Xingpeng, Meng Meifang, Cao Mingyue, Zhang Qiao, 2024. Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone. Earth Science, 49(6): 2071-2084. doi: 10.3799/dqkx.2022.480
    shu

    Time Limit of Dextral Strike-Slip in Cenozoic of Liaodong Bay Section of Tan-Lu Fault Zone

    doi: 10.3799/dqkx.2022.480
    • 1.

      State Key Laboratory of Deep Oil and Gas, China University of Petroleum, Qingdao 266580, China

    • 2.

      School of Earth Science and Technology, China University of Petroleum, Qingdao, 266580, China

    • 3.

      Tianjin Branch, CNOOC, Tianjin 300452, China

    • 4.

      Tarim Oilfield Company, PetroChina, Korla 841000, China

    • Received Date: 2022-09-18
      Available Online: 2024-07-11
    • Publish Date: 2024-06-25
      Abstract
    • The Tan-Lu Fault Zone has undergone a complex evolutionary process during Cenozoic, and the controversy is mainly focused on the period of the beginning of dextral strike-slip. In this paper, based on various geological and geophysical data and previous research results, taking the Liaodong Bay Section in Bohai Sea as an example, the time limit of dextral strike-slip activity of the Tan-lu fault zone is systematically discussed from both tectonic and sedimentological aspects based on various evidence. The results show that the dextral strike-slip activity of the Liaodong Bay Section of the Tan-Lu fault zone cut and modified the early (Kongdian-the third member of Shahejie formation depositional period) extensional faults, the R-shear fracture was formed in the Late Oligocence Dongying Formation depositional period, and the strike-slip derived structures were mainly developed in the Dongying Formation depositional period until now. The dextral strike-slip activity in the Liaodong Bay Section of the Tan-Lu fault zone staggered the sedimentary bodies formed in Early and Middle Paleogene(Kongdian-Shahejie formation depositional period), and the syndepositional dextral strike-slip activity led to the development and spreading of fish-jumping sand bodies, axial or oblique sand bodies, and the local depression formation controlled by the pressure release effect of bending strike-slip fault. The dextral strike-slip in Cenozoic of the Liaodong Bay Section of the Tan-Lu fault zone was mainly during the depositional period of the Dongying Formation in the Late Oligocene of the Paleogene, and then gradually weakened and continued until now.

       

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