›› 2018, Vol. 32 ›› Issue (2): 165-168.

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Evaluation of Slide in a Weathered Granite Slope

ZHOU  Xing-Long-1, ZHOU  Li-Hong-2, ZHOU  Xing-Hua-3   

  1. (1.Guangdong Engineering Investigation Institute, Guangzhou 510510;
    2.Guanzhou Jintu Geotechnical Engineering Co., Ltd., Guangzhou 510510;
    3.Gannan Geological Survey Division, Jiangxi Geology and Mineral Exploration and Development Bureau, Ganzhou 341000)
  • Received:2017-05-18 Revised:2017-05-26 Online:2018-04-30 Published:2018-05-09

Abstract: The granite is a common bedrock type that is widely distributed in Guangdong Province which is underneath approximate 40% of the land area. The weathered granite in this region has a thick deposit depth, low shear strength when it soaks in the water and prone to develop landslide. A landslide in Maogu Village, Taibao Township of Lianshan County is a typical landslide in the weathered granite residual soils. This paper presents the landslide evaluation results and factors that cause the slide from the development of the slide and geological conditions.

Key words: Granite Bedrock, Landslide, Factors Inducing the Slide