Based on the monitoring data of landslide deep deformation obtained with inclinometer, the original deformation mechanism for sliding zone of talus slide is studied.
根据钻孔倾斜仪深部变形监测资料，研究了清江水布垭工程堆积体滑坡滑带的变形机制。
Investigation indicates that: talus material, residual deposit and strong weathering bedrock are material base of clastic flow landslide;
调查分析表明：残坡积物与强风化基岩是碎屑流滑坡的物质基础；
应用推荐