Volume 29 Issue 6
Dec.  2023
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Article Navigation >  Journal of Geomechanics  > 2023  >  29(6): 879-887
NIU W Z，HE F B，LIU Z H，et al.，2023. Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity[J]. Journal of Geomechanics，29（6）：879−887 doi: 10.12090/j.issn.1006-6616.2023032
Citation: NIU W Z，HE F B，LIU Z H，et al.，2023. Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity[J]. Journal of Geomechanics，29（6）：879−887 doi: 10.12090/j.issn.1006-6616.2023032
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Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity

doi: 10.12090/j.issn.1006-6616.2023032
  • 1.

    Beijing Institute of Geological Survey, Beijing 100097, China

  • 2.

    Beijing Municipal Staff Innovation Studio (Urban Geology, Active Structure and Monitoring), Beijing 100097, China

  • 3.

    Development and Research Center of China Geological Survey, Beijing 100037, China

Funds:  This research is financially supported by the Beijing Geological Survey Project (Grant No. PXM2018-158203-000014) and the Fund of the Beijing Natural Science Foundation（Grant No.8234070）
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  • Received: 2023-03-15
  • Revised: 2023-10-10
    • Available Online: 2024-01-02
    Abstract
  • The Nanyuan–Tongxian fault is the boundary fault between the Beijing depression and the Daxing uplift, also the primary seismic-controlling fault of the Beijing M $ 6{\dfrac{1}{2}}$ earthquake in 1665. Its activity is of great significance to land planning and geological disaster prediction in Beijing. Using high-precision gravity, longitudinal-wave and shear-wave seismic comprehensive exploration profiles, and composite borehole geological profiles, this study investigated the geometric characteristics and activity of the northeastern section of the Nanyuan–Tongxian fault. The results show that after passing through Pingjiatuan Village in Tongzhou District, the fault turns to a nearly east-west direction, trending north with a dip angle of 56° to 75°. The new activity in the northeastern section exhibits characteristics of a normal fault, with an estimated buried depth of about 21.6 m, indicating it as a late Pleistocene active fault. The findings demonstrate that the activity age of the northeast section of the Nanyuan–Tongxian fault differs from that of the middle and southwestern sections, providing crucial geological foundations for the spatial planning and disaster reduction systems in the Beijing region.

     

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