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Volume 32 Issue 5
Oct 2021
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Journal of Earth Science  > 2021  >  32(5): 1069-1078.
Yuandong Huang, Chong Xu, Xiaolong Zhang, Chunji Xue, Shiyuan Wang. An Updated Database and Spatial Distribution of Landslides Triggered by the Milin, Tibet Mw6.4 Earthquake of 18 November 2017. Journal of Earth Science, 2021, 32(5): 1069-1078. doi: 10.1007/s12583-021-1433-z
Citation: Yuandong Huang, Chong Xu, Xiaolong Zhang, Chunji Xue, Shiyuan Wang. An Updated Database and Spatial Distribution of Landslides Triggered by the Milin, Tibet Mw6.4 Earthquake of 18 November 2017. Journal of Earth Science, 2021, 32(5): 1069-1078. doi: 10.1007/s12583-021-1433-z
shu

An Updated Database and Spatial Distribution of Landslides Triggered by the Milin, Tibet Mw6.4 Earthquake of 18 November 2017

doi: 10.1007/s12583-021-1433-z
  • 1.

    National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 3.

    Key Laboratory of Compound and Chained Natural Hazards Dynamics (Under Construction), Ministry of Emergency Management of China, Beijing 100085, China

  • 4.

    Sichuan Earthquake Agency, Chengdu 610041, China

More Information
  • Corresponding author: Chong Xu: xc11111111@126.com
  • Received Date: 29 Nov 2020
  • Accepted Date: 09 Feb 2021
  • Publish Date: 01 Oct 2021
    Abstract
  • The Mw6.4 earthquake on November 18, 2017 in Milin County, Nyingchi City, Tibet triggered thousands of landslides. By comparing visual interpretation of satellite images acquired shortly before and after the earthquake and field survey, we have created a new landslide database which includes 3 130 coseismic landslides, each with an area of 0.01 to 4.35 km2. Six factors (elevation, slope angle, slope aspect, lithology, distance from the epicenter and distance from the seismogenic fault) were selected to correlate with the coseismic landslides. In addition, the area and density of landslides were counted as indicators. Results show that most landslides occurred where the elevation is between 2 000-3 000 m, with a 40°-50° slope angle and S, E or SE slope aspect, schist or gneiss lithologies, 10-15 km from the epicenter, and 5 km within the seismogenic fault. Most of the landslides, triggered by the Mw6.4 earthquake, are concentrated near the seismogenic fault rather than at the epicenter, indicating that the seismogenic structure is more influential than the location of the epicenter. Our findings may differ from other landslide database due to temporal image acquisition, interference from weather, and image resolution.

     

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