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    Volume 50 Issue 1
    Jan.  2025
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    Yu Huayu, Dong Youpu, Yu Liang, Zhang Dongyue, Wang Dan, Duan Jiaxin, Ren Yangyang, Li Jiangtao, 2025. Relative Tectonic Activity of Puduhe Fault in Central Yunnan. Earth Science, 50(1): 336-348. doi: 10.3799/dqkx.2022.172
    Citation: Yu Huayu, Dong Youpu, Yu Liang, Zhang Dongyue, Wang Dan, Duan Jiaxin, Ren Yangyang, Li Jiangtao, 2025. Relative Tectonic Activity of Puduhe Fault in Central Yunnan. Earth Science, 50(1): 336-348. doi: 10.3799/dqkx.2022.172

    Relative Tectonic Activity of Puduhe Fault in Central Yunnan

    doi: 10.3799/dqkx.2022.172
    • Received Date: 2022-02-22
      Available Online: 2025-02-10
    • Publish Date: 2025-01-25
    • The Xianshuihe-Xiaojiang fault zone diverges into several SN-trending branch faults in central Yunnan, among which the Puduhe fault has triggered earthquakes of magnitude more than 5 for many times, but its spatial distribution characteristics of tectonic activity are not clear. Because geomorphic index is very sensitive to tectonic activity, it can well indicate the distribution characteristics of tectonic activity. In order to study the distribution characteristics of tectonic activity of the Purduhe fault, 41 basins in the Purduhe fault region were extracted by using digital elevation model (DEM) with a resolution of 30 m. The basin is divided into three sections: north section (Sayingpan-Fumin Section), middle section (Fumin-Jinning Section) and south section (Jinning-Eshan Section). Seven geomorphic indices including hypsometric curve and hypsometric integral (HI), asymmetric factor (AF), basin shape index (BS), the ratio of valley floor width to valley height (VF), normalized stream-length gradient (SLK), sinuosity of the mountain front (Smf) and the steepness index(Ksn)were obtained through analysis. The results show that the spatial variation characteristics of geomorphic indices of the Puduhe fault are not affected by non-structural factors (precipitation and lithology), but they are mainly affected by tectonic activities. The relative tectonic activity of the Puduhe fault gradually decreases from north to south, and the tectonic activity of the east side of the fault is slightly weaker than that of the west side. The structural activity of the Puduhe fault is weaker than that of the Xiaojiang fault, indicating that during the extrusion process of the Sichuan-Yunnan block, the highly active area is mainly concentrated in the boundary fault zone.

       

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