摘要
乱石岗滑坡位于汉源罗卜岗新县城规划区中部,滑坡体积110.7×104m3,属大型滑坡,现今滑坡体在天然或暴雨状态下处于稳定状态。对滑坡形成机制进行深了入分析。
The Luanshigang landslide is a large landslide with a volume of 110.7×104 m3 in the new seat of Hanyuan County Town.At present it is in stability.This paper makes an approach to its genetic mechanism.
出处
《四川地质学报》
2009年第3期303-305,共3页
Acta Geologica Sichuan
关键词
滑坡
形成机制
诱发作用
四川汉源乱石岗
landslide
genetic mechanism
induced
Luanshigang
Hanyuan
Sichuan
