安徽地质2016，Vol.26Issue(2)：127-131,5.
皖南山区典型顺层滑坡形成机制研究
STUDY ON FORMATION MECHANISM OF TYPICAL BEDDING LANDSLIDE IN THE MOUNTAINOUS AREA OF SOUTH ANHUI
黄健敏 1潘国林 1罗云丰2
作者信息
- 1. 安徽省公益性地质调查管理中心，安徽合肥 230001
- 2. 成都理工大学地质灾害防治与地质环境保护国家重点实验室，四川成都 610059
- 折叠
摘要
Abstract
The Niaoqueping landslide is a typical bedding rocky landslide in the South Anhui mountainous area, whose deformational destruction is in a mode of sliding-bending and in a process divided into three stages as initial slope formation, surface unloading rebound, overlying rockmass movement, underlying rockmass uplift and bending, sliding face overall taking form and landslide mass instability and destruction. The landslide formed 200m along river, and 700m in lengthwise direction, and about a accumulation body of 200×104m3, jammed the Dayuan River and rechanneled it.关键词
顺层滑坡/形成机制/鸟雀坪滑坡/皖南山区Key words
bedding landslide/Niaoqueping landslide/South Anhui mountainous area/formation mechanism分类
天文与地球科学引用本文复制引用
黄健敏,潘国林,罗云丰..皖南山区典型顺层滑坡形成机制研究[J].安徽地质,2016,26(2):127-131,5.
