摘要
重庆市麻柳嘴滑坡是一顺层发育的大型滑坡 ,总体积 2 5 74× 10 4m3 ,因其体积大 ,加之位于三峡工程库区而倍受各方的关注。麻柳嘴滑坡是典型的暴雨诱发型滑坡 ,文章在结合分析滑坡形态、结构特征的基础上 ,综合考虑了影响滑坡变形复活的主要因素 ,对滑坡的形成机制进行了有益探讨 ,并总结了滑坡的变形破坏特征 ;在滑坡位移监测的基础上 ,分析了滑坡的稳定现状及变形发展趋势 。
Maliuzui Landslide is a large bedding slip landslide And its volume is up to 2574×10 4 m 3. Why the landslide is soconcentrated on is that it is located in the Three Gorges Reservoir Area of the Yangtse River and its large volume. The landslide is a typical storm induced landslide. In this paper, the configuration and structure characteristics of the landslide, and the influencing factors of the landslide deformation and revival are introduced. Its genetic mechanism and deformation and failure character are analyzed,and the stability state and the deformation trend of the landslide are also analyzed, which provide the basis for landslide control project.
出处
《中国地质灾害与防治学报》
CSCD
2001年第4期53-57,共1页
The Chinese Journal of Geological Hazard and Control
关键词
滑坡
变形
复活
机制
landslide
deformation
revival
genetic mechanism
