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WANG Xiuqin，NIU Quanfu，WANG Hao，et al. Risk assessment of landslides induced by the Ms6.2 earthquake in Jishishan, Gansu Province[J]. The Chinese Journal of Geological Hazard and Control，2025，36(1): 169-181. DOI: 10.16031/j.cnki.issn.1003-8035.202405010
Citation: WANG Xiuqin，NIU Quanfu，WANG Hao，et al. Risk assessment of landslides induced by the Ms6.2 earthquake in Jishishan, Gansu Province[J]. The Chinese Journal of Geological Hazard and Control，2025，36(1): 169-181. DOI: 10.16031/j.cnki.issn.1003-8035.202405010
shu

Risk assessment of landslides induced by the Ms6.2 earthquake in Jishishan, Gansu Province

  • 1.

    The Map Institute of Gansu Province, Lanzhou, Gansu　730000, China

  • 2.

    School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu　730050, China

  • 3.

    Gansu Provincial Institute of Surveying and Mapping, Lanzhou, Gansu　730000, China

  • 4.

    The Third Geological and Mineral Exploration Institute of Gansu Provincial Geological and Mineral Exploration and Development Bureau, Lanzhou, Gansu　730050, China

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  • Received Date: May 07, 2024
  • Revised Date: September 04, 2024
  • Accepted Date: January 02, 2025
  • Available Online: January 05, 2025
    Graphical Abstract
    • Abstract

  • On December 18, 2023, at 23:59, a magnitude Ms6.2 earthquake occurred in Jishishan County, Gansu Province, resulting in significant casualties and triggering numerous secondary geological disasters such as landslides and collapses. Utilizing high-resolution satellite imagery from before and after the earthquake, this study employs a MaxEnt model, constructed with visually interpreted disaster points and a set of impact factor characteristics, to assess the post-earthquake landslide hazard post-earthquake landslide hazard. The research conclusions are as follows: 1) Earthquake-induced landslide disasters are predominantly distributed within sunny slopes at elevations of 1800 to 2300 m and slope gradient of 20° to 25°, extensively across areas 1.5 km from roads, 1.7 km from fault zones, and within 5 km of the earthquake’s epicenter. The majority of the disasters occurred in cropland and loam areas with higher population density in the earthquake region. 2) The main influencing factors for earthquake-induced landslides determined by factor contribution rates, permutation importance, test benefit values, AUC values, and regularization training gain value were comprehensively determined as follows: Distance from the fault zone, Elevation, and Population density; 3) Based on the constructed MaxEnt model, it is found that there is a good consistency between the extremely high and high-risk areas of landslide disasters in the earthquake zone and the seismic intensity. Among them, the extremely high and high-risk areas are mainly distributed in the intensity Ⅷ zone, with an area of 5.368km2, accounting for 77.82% of the total area of the extremely high and high-risk zones. The low and very low-risk areas are mainly distributed in the intensity Ⅵ and Ⅶ zones, accounting for 92.80% of the total area of the study region. This study constructs the MaxEnt model based on the importance analysis of impact factors to evaluate the landslide hazard in the earthquake area, providing references for post-disaster reconstruction in the earthquake zone.

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