渤海南部地区潜山构造差异与成因机制

吴庆勋; 韦阿娟; 王粤川; 彭靖淞; 肖述光; 高坤顺; 郭永华; 邓辉

doi:10.3799/dqkx.2018.578

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3698-3708

Wu Qingxun, Wei Ajuan, Wang Yuechuan, Peng Jingsong, Xiao Shuguang, Gao Kunshun, Guo Yonghua, Deng Hui, 2018. Tectonic Difference and Genetic Mechanism of Buried Hill in Southern Bohai Area. Earth Science, 43(10): 3698-3708. doi: 10.3799/dqkx.2018.578

Citation:

Wu Qingxun, Wei Ajuan, Wang Yuechuan, Peng Jingsong, Xiao Shuguang, Gao Kunshun, Guo Yonghua, Deng Hui, 2018. Tectonic Difference and Genetic Mechanism of Buried Hill in Southern Bohai Area. Earth Science, 43(10): 3698-3708. doi: 10.3799/dqkx.2018.578

Citation:

Wu Qingxun, Wei Ajuan, Wang Yuechuan, Peng Jingsong, Xiao Shuguang, Gao Kunshun, Guo Yonghua, Deng Hui, 2018. Tectonic Difference and Genetic Mechanism of Buried Hill in Southern Bohai Area. Earth Science, 43(10): 3698-3708. doi: 10.3799/dqkx.2018.578

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Tectonic Difference and Genetic Mechanism of Buried Hill in Southern Bohai Area

doi: 10.3799/dqkx.2018.578

1.
CNOOC Co. Ltd. Tianjin Branch, Tianjin 300459, China
2.
CNOOC Energy Technology & Services-Engineering Technology Co., Tianjin 300459, China

Received Date: 2017-10-15
Publish Date: 2018-10-20

Abstract

Abstract

At present, there barely have studies on the stratigraphic structure and tectonic evolution of the buried hill in southern Bohai Sea area. Combined with the 3D seismic data and well data, this study was carried out on the fault types of the buried hills, the structural styles of the buried hills and the genesis and evolution of the buried hills and dynamic background of the buried hills. The results show that the Tanlu strike-slip faults trending near SN direction and the extension faults trending near EW direction jointly controlled the stratigraphic distribution of the buried hill strata, thus affecting the structural differences of the buried hill strata. The Tanlu strike-slip fault trending near SN direction was transform fault in Indo-Chinese epoch, which regulated the compressive strength of the both sides of east and west. The compressive deformation is relatively weak on the west side of the west branch of the Tanlu strike-slip fault, which led to the general development of "thin based" or "bald based". Paleozoic structures that are dominatated by three-layer-structures of Mesozoic+Paleozoic+Precambrian. The compressive deformation on the east side of the west branch was relatively strong, which led to the development of strong uplift, where the Paleozoic stratum has been completely eroded and two-layer-structures of Mesozoic+Precambrian dominate. The reverse faults trending near EW direction were thrust faults in Indo-Chinese epoch, and developed extension and inversion in late Yanshan epoch, in which Paleozoic still remains in upthrow side of the fault but almost completely eroded in downthrow side of the fault. The diversity of the amount of lateral extrusion shrinkage was the main cause for the difference of structural styles of the buried hills in the study area.
- southern Bohai Sea area,
- tectonic evolution,
- strike-slip fault,
- inverted fault,
- Tanlu fault,
- genetic mechanism,
- Paleozoic,
- petroleum geology

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References(73)

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