Volume 28 Issue 3
Jun.  2022
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Article Navigation >  Journal of Geomechanics  > 2022  >  28(3): 480-491
DENG Lujia, WU Kongyou, JIAO Hongyan, et al., 2022. Paleogene fault system in the Xianhe mining area, Dongying Sag, Bohai Bay Basin and its evolution. Journal of Geomechanics, 28 (3): 480-491. DOI: 10.12090/j.issn.1006-6616.2021139
Citation: DENG Lujia, WU Kongyou, JIAO Hongyan, et al., 2022. Paleogene fault system in the Xianhe mining area, Dongying Sag, Bohai Bay Basin and its evolution. Journal of Geomechanics, 28 (3): 480-491. DOI: 10.12090/j.issn.1006-6616.2021139
shu

Paleogene fault system in the Xianhe mining area, Dongying Sag, Bohai Bay Basin and its evolution

doi: 10.12090/j.issn.1006-6616.2021139
  • 1.

    School of Geosciences, China University of Petroleum (East China), Qingdao 266580, Shandong, China

  • 2.

    Xianhe Oil Production Plant, Shengli Oilfield Company, SINOPEC, Dongying 257100, Shandong, China

Funds:

the Class A Strategic Priority Science and Technology Project of Chinese Academy of Sciences XDA14010301

More Information
  • Received: 2021-10-13
  • Revised: 2022-04-07
    Abstract
  • Controlled by the dual dynamic background, the superposition of Paleogene extension and strike-slip is obvious in the Xianhe mining area, Dongying sag, Bohai Bay Basin. It is of great significance for oil and gas exploration to clarify the superposition of the fault system. This paper is based on high-precision seismic data and drilling data. We conducted in-depth research on the fracture types and combination styles, fracture superposition, fracture activity and evolution, and regional dynamics background by using an integrated interpretation of well-log and seismic data, structural style identification, quantitative characterization of faulting and balanced profile recovery. The results show that two fracture systems, extensional and extensional–strike-slip, are developed in the Paleocene of the Xianhe mining area, and the extensional–strike-slip fractures are formed by the superposition of the previous extensional fractures with slip action. Regional faulting reached two peaks in the Paleogene, one is in the middle of Member 3 of the Shahejie Formation and the other is in the early Dongying Formation. Under the superposition of extensional and strike-slip stress, the faults in the Xianhe mining area experienced five major evolution stages: initial extensional stage (Ek–Es4), intensely extensional stage (Es3x–Es2x), strike-slip stage and weak extensional stage (Es2s–Es1), reactivation and extensional stage (Ed), and stabilization stage (N–Q).

     

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