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.
出处
《水土保持通报》
CSCD
北大核心
1997年第3期31-36,共6页
Bulletin of Soil and Water Conservation
关键词
长武王东沟
滑坡成因
地下水
人类活动
Wangdong gully in Changwu county,Shaanxi province
landslide development
underground water
human being action
