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Volume 38 Issue 3
Jun.  2019
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Article Navigation >  CARSOLOGICA SINICA  > 2019  >  38(3): 418-426
LI Zhihao, XU Guangquan, YU Shitao, GAO Jialin, ZHANG Haitao. Study on the development characteristics and formation mechanism of karst collapse development in Shungeng mountain, Huainan City[J]. CARSOLOGICA SINICA, 2019, 38(3): 418-426. doi: 10.11932/karst2018y09
Citation: LI Zhihao, XU Guangquan, YU Shitao, GAO Jialin, ZHANG Haitao. Study on the development characteristics and formation mechanism of karst collapse development in Shungeng mountain, Huainan City[J]. CARSOLOGICA SINICA, 2019, 38(3): 418-426. doi: 10.11932/karst2018y09
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Study on the development characteristics and formation mechanism of karst collapse development in Shungeng mountain, Huainan City

doi: 10.11932/karst2018y09
  • 1.

    Anhui University of Science and Techology,Huainan, Anhui 232001,China/The 1st Geological Brigade of Jiangsu & Mineral Exploration Bureau,Nanjing,Jiangsu 210041, China

  • 2.

    Anhui University of Science and Techology,Huainan, Anhui 232001,China

  • Publish Date: 2019-06-25
    Abstract
  • The Shungeng mountain of Huainan City is located in the southern margin of North China plate. The karst landforms are well developed and the geological hazards of karst collapse occur frequently, which bring great potential disasters to people’s life and property in the region. Based on the karst field geological investigation, the statistics of karst collapse characteristics and the analysis of structural geology and hydrogeological conditions in the exposed and cover areas of carbonate rocks in the area, the karst collapse development mechanism in this area is summarized. The results show that the development of karst collapse in the exposed carbonate area is mainly influenced by the multi-phase tectonic movements and lithologic assemblage in this area; and the extension of the karst collapses are mainly in NW direction and most of them are located at the interface between soluble and non-soluble rocks, of which the formation mechanism is mainly structure destruction and underground erosion. The development of karst collapse in covered carbonate rock area is mostly caused by the increase of ground structures, which leads to the increase of static load and the collapse induced by strong drainage in the mining area. The formation mechanism is dominated by effective stress failure and vacuum inhaling corrosion.

     

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