长武王东沟滑坡成因分析  

Study on Landslide Development of Wangdong Gully in Changwu County,Shaanxi Province

作　　者：武春龙[1] 

机构地区：[1]中国科学院水利部水土保持研究所

出　　处：《水土保持通报》1997年第3期31-36,共6页Bulletin of Soil and Water Conservation

摘　　要：该文主要研究了长武王东沟古滑坡分布和分类，以及现代滑坡的发育条件。通过现代滑坡的典型实例调查，系统分析了地形条件、新构造应力场、黄土地层、大气降水与地下水运动。The development, distribution and classification of paleolandslide of Wangdong gully in Changwu county, Shaanxi province are mainly studied. According to typical investigation and systematical analysis, the result shows that it is the factors of geological structure, geomorphological forms,neotectonic stress fields, the movement of underground water and human being action that affect the development of modern landslide.

关 键 词：长武王东沟 滑坡成因 地下水 人类活动 

分 类 号：P642.22[天文地球—工程地质学]