川主寺尕里台滑坡形成机制分析  

Genetic Mechanism for the Galitai Landslide at the Chuanzhu Temple

作　　者：王影[1] 陈国辉[1] 钟声[1] 王晓东[1] 

机构地区：[1]四川省地质工程勘察院,成都610072

出　　处：《四川地质学报》2009年第4期446-448,共3页Acta Geologica Sichuan

摘　　要：尕里台滑坡位于松潘县北西约39km,在哲波河上游尕里台支沟右岸Ⅰ级阶地边缘谷坡中下部,为体积约10×104m3的中型滑坡。滑坡体在天然或暴雨状态下处于不稳定状态,现根据所掌握的资料,对滑坡形成机制进行分析。The Galitai landslide is located at about 39 km northwest of Songpan County Town, lying in the middle-lower part of terrace Ⅰ of the right bank of the Galitai valley in the upper reaches of the Zhebo River with the volume of about 10 × 10^4m^3. This paper makes an approach to the genetic mechanism for the landslide.

关 键 词：滑坡 形成机制 诱发作用 尕里台 

分 类 号：P642.22[天文地球—工程地质学]