摘要
剧冲式滑坡是具有剧动启程、高速运行、碰撞解体及冲击成坝的高速岩质滑坡。本文以川西青衣江上游宝兴河大板桥滑坡为典型研究对象， 论述了剧冲式高速岩质滑坡地质特性及滑坡坝的形成演化过程， 为利用滑坡体构筑大坝提供科学依据。
Landslide with acute moving and high colliding speed is described as the process of violent starting, highspeed motion, colliding disintegration and dam ramming of landslide mass after failure Taking the Dabanqiao landslide on the upper reaches of the Baoxin river in the Sichuan Province as an example, the geological features of rocky highspeed landslide and the evlution process of landslide dam are studied thoroughly and systematically based upon data and information from field investigation, thus provide the scientific basis for stability evaluation of landslide dam
出处
《中国地质灾害与防治学报》
CSCD
1999年第3期28-36,共9页
The Chinese Journal of Geological Hazard and Control
基金
国土资源部岩土工程开放研究实验室基金
