摘要
根据工程地质分析的方法对大渡河官料河昔木呷沟泥石流的形成环境、基本特征、形成演化过程及机制模型、泥石流沟岸坡稳定性评价等进行了分析 ,并对泥石流活动趋势做出科学的评价预测。对工程建设中的泥石流分析有着积极的指导作用。
In this paper,the authors analyse the formation conditions,basic characteristics and the formation and evolution steps of the Ximuxia gully debris flow in the branch(Guanliao river)by the engineering geology analysis.The authors evaluate the mechanism model and the slope stability of the debris flow gully and makes a scientific prediction for the trend of the debris flow activities.This has an active guiding meaning in analysing the debris flows in engineering constructions.
出处
《地质灾害与环境保护》
2002年第2期26-29,58,共5页
Journal of Geological Hazards and Environment Preservation
