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    Volume 48 Issue 8
    Aug.  2023
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    Article Contents
    Zhou Jie, Hu Lin, Hu Gaowei, Liao Jun, Guo Li, Liu Zheng, 2023. Characteristics of Middle-Deep Faults in the Southern Segment of the Eastern Belt of Yinggehai Basin and Their Controlling Effect on Natural Gas Accumulation. Earth Science, 48(8): 3021-3030. doi: 10.3799/dqkx.2022.479
    Citation: Zhou Jie, Hu Lin, Hu Gaowei, Liao Jun, Guo Li, Liu Zheng, 2023. Characteristics of Middle-Deep Faults in the Southern Segment of the Eastern Belt of Yinggehai Basin and Their Controlling Effect on Natural Gas Accumulation. Earth Science, 48(8): 3021-3030. doi: 10.3799/dqkx.2022.479

    Characteristics of Middle-Deep Faults in the Southern Segment of the Eastern Belt of Yinggehai Basin and Their Controlling Effect on Natural Gas Accumulation

    doi: 10.3799/dqkx.2022.479
    • Received Date: 2022-10-15
    • Publish Date: 2023-08-25
    • The purpose of this paper lies in clarifying the characteristics of faults in middle-deep layers in the southern segment of the eastern belt of Yinggehai Basin and their controlling effect on natural gas accumulation. Based on the new 3D seismic data, the faults in middle-deep layers in the southern segment of the eastern belt of Yinggehai Basin are described precisely for the first time. Combined with the characteristics of regional tectonic evolution, the types, shapes and activities of the faults are analyzed, and the controlling effect of the faults on natural gas accumulation is discussed. The results show that the Eocene-Early Miocene Yinggehai Basin is in the tectonic deformation stress field caused by left strike-slip. Located in the strike-slip transition zone of the No. 1 fault, the southern segment of the eastern belt of Yinggehai Basin develops three groups of tension-torsion (partialcompression-torsion) strike-slip faults. On the plane, the faults are NW-SE trending, with a left-lateral and right-step distribution. On the section, three groups of the faults are steep in occurrence, and present fault-step-like style and flower-like structures locally. The faults are mainly active in three phases: (1)Eocene-Early Oligocene, (2)Early and Mid-Late Oligocene, (3)Early Miocene, characterized by "early faults early senescence". The multi-stage activities of the faults in middle-deep layers control the development of land source deltas and hydrocarbon sources in the Yacheng Formation, the formulation of the "second step" gas accumulation background, the spatial distribution of sandstone in the Sanya Formation and the formation of traps. With a good match of production, migration and accumulation, the middle-deep layer in the southern section of the eastern belt of Yinggehai Basin is expected to become a natural gas accumulation area of 100 billion cubic meters in the Yinggehai Basin.

       

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