泾河南岸崩岸型滑坡的发育规律  

Development Pattern of Slumping Bank Type Landslides at the South Bank of Jinghe, Shaanxi Province

作　　者：范立民[1] 岳明[2] 冉广庆[2] 

机构地区：[1]陕西省煤田地质局,陕西西安710054 [2]陕西省煤田地质局131队,陕西韩城715400

出　　处：《中国煤田地质》2004年第5期33-35,42,共4页Coal Geology of China

摘　　要：关中地区滑坡灾害主要发生在河流沿岸,产生地毁人伤的严重后果。经对泾河南岸黄土台塬地区滑坡的形成条件、发育特征、影响因素的分析,认为滑坡的形成除自然原因外,人为削坡、工程活动等因素是诱发滑坡的主要因素。通过对典型滑坡的分析,提出了防治措施。Landslides in Guanzhong Area are mainly took place along rivers usually cause serious consequences of land breakdown and casualties. After analyses of forming condition, development pattern and influential factor, authors think other than natural causes, artificial slope cutting and other engineering activities are main landslide inducing factors. Through typical landslide analysis, the paper put forward landslide control measures.

关 键 词：滑坡 发育特征 黄土台塬 泾河南岸 

分 类 号：P642.22[天文地球—工程地质学]