Characteristics and Formation Mechanism of High Slope Landslide Induced by Wenchuan Earthquake in Miaoba County of Dujiangyan City
详细信息
- 责任者：Gou Fugang (State Key Laboratory of Geo-hazard Prevention and Geo-Environment Protection ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Wang Yunsheng
- 刊名：Journal of Engineering Geology
- 出版年：2012
- 卷期：20(1)
- 关键词：滑坡 ; landslides ; 四川 ; Sichuan Province
- 页码：p.21-29
- 图表：9 illus., 12 refs.
- 分类号：1702
- issnNo：ISSN1004-9665
- isbnNo：CN11-3249/P
摘要
The Miaoba landslide is a typical representative.The Miaoba landslide lies in the middle of the central fault zone of Longmen Mountains.The intensity of the landslide area is Ⅺ.The landslide volume is about 113×104m3.Through the field investigation and synthetic analysis,this paper strives to reveal its characteristics and formation mechanism.It takes a detailed partition of the landslide. Based on the analysis of formation mechanism of the landslide,this paper obtains that the functions of coupling dynamic of the internal and external earth are the reasons of forming the high landslide induced by earthquake.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |