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    Volume 49 Issue 2
    Feb.  2024
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    Article Navigation >  Earth Science  > 2024  >  49(2): 759-780
    Wang Zijun, Yao Wenqian, Liu-Zeng Jing, Shao Yanxiu, Wang Wenxin, Shen Xuwen, Gao Yunpeng, Xu Jing, 2024. Application of Tectonic Geomorphology Method for Constraining the Slip Rate Uncertainty and Implication of Strike-Slip Faults: An Example from the Haiyuan Fault Zone. Earth Science, 49(2): 759-780. doi: 10.3799/dqkx.2022.405
    Citation: Wang Zijun, Yao Wenqian, Liu-Zeng Jing, Shao Yanxiu, Wang Wenxin, Shen Xuwen, Gao Yunpeng, Xu Jing, 2024. Application of Tectonic Geomorphology Method for Constraining the Slip Rate Uncertainty and Implication of Strike-Slip Faults: An Example from the Haiyuan Fault Zone. Earth Science, 49(2): 759-780. doi: 10.3799/dqkx.2022.405
    shu

    Application of Tectonic Geomorphology Method for Constraining the Slip Rate Uncertainty and Implication of Strike-Slip Faults: An Example from the Haiyuan Fault Zone

    doi: 10.3799/dqkx.2022.405
    • 1.

      Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China

    • 2.

      State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

    • 3.

      The Second Monitoring and Application Center, China Earthquake Administration, Xi'an 710054, China

    • Received Date: 2022-12-13
    • Publish Date: 2024-02-25
      Abstract
    • The fault slip rate of is critical for understanding strain partitioning within a fault system and assessing seismic hazard. Tectonic geomorphology method can be used in constraining Quaternary slip rates in general. In the active fault system of Tibetan Plateau, the Haiyuan Fault Zone accommodates part of Indo-Asian convergence and its slip rate provides reference for understanding the mechanics of continental deformation. Thus, several slip rate studies have been carried out along the Haiyuan fault during the past 3 decades and the results range from 2.3 mm/a to 16 mm/a, which caused controversy and confusion. Based on a review of the previous studies, we point out that the main reason for the difference in previous studies is the choice of upper terrace and lower terrace reconstruction models. We infer that the upper and lower bound of slip rates are obtained based on the two models in general, which cannot be simply equated with the real slip rate value. When there is a lack of observational data to distinguish the reliability of the two models, a combination of upper and lower terrace abandonment age constraints can be used to bracket the slip rate. The method shows the respect and recognition of the objective uncertainty in the calculation process of slip rate. In addition, the evaluation of slip rates of Haiyuan fault zone can provide a basis for the identification of two end models of the Tibetan Plateau based on the intro-block faults deformation.

       

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