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    Volume 48 Issue 6
    Jun.  2023
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    Tang Daqing, Chen Honghan, Geng Feng, Qi Rong, Jiang Hua, Guzailinuer·Aierken, 2023. Characteristics of Intraplate Small-Displacement Strike-Slip Faults: A Case Study of Tarim, Sichuan and Ordos Basins. Earth Science, 48(6): 2067-2086. doi: 10.3799/dqkx.2023.037
    Citation: Tang Daqing, Chen Honghan, Geng Feng, Qi Rong, Jiang Hua, Guzailinuer·Aierken, 2023. Characteristics of Intraplate Small-Displacement Strike-Slip Faults: A Case Study of Tarim, Sichuan and Ordos Basins. Earth Science, 48(6): 2067-2086. doi: 10.3799/dqkx.2023.037

    Characteristics of Intraplate Small-Displacement Strike-Slip Faults: A Case Study of Tarim, Sichuan and Ordos Basins

    doi: 10.3799/dqkx.2023.037
    • Received Date: 2022-09-07
    • Publish Date: 2023-06-25
    • Intraplate small-displacement strike-slip faults are widely developed and play an important role in controlling hydrocarbon migration and accumulation in sedimentary basins. It compares geometric characteristics of small-displacement strike-slip faults in Tarim, Sichuan, and Ordos basins in western and central China and shows the similarities and differences in structural style. It also discusses the geological setting that controls the small-scale faults evolution in these craton basins. The comparison shows that Tarim, Sichuan, and Ordos basins have four aspects of characteristics. (1) Intraplate small-displacement strike-slip faults are developed in the central and northern parts of Tarim basin, in the central part of Sichuan basin, and in the southern and northern Hangjinqi parts of Ordos basin. (2) The strike-slip faults in these three major basins show obvious linear features, but their location in each basin varies. The central and northern parts of the Tarim basin can be divided into five strike-slip fault development areas with different characteristics. The strike-slip faults in central part of Sichuan basin are irregular network, and the strike-slip faults in Jinghe area of Ordos basin are mainly NEE- trending and partially NW-trending. (3) The strike-slip fault in these three basins show high dips. In Tarim basin, fault geometries in cross-section include linear, positive flower and negative flower structures that developed in pure strike-slip, transtension, transpression and superposition or inversion. The strike-slip faults in the central Sichuan basin are mostly upright with few flower structures. The strike-slip faults in Jinghe area of Ordos basin have the characteristic of composite flower structure or "flower on flower" because of strike-slip inversion or reactivation.

       

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