Distribution Characteristics of Landslides and Debris Flows in the Wenchuan Earthquake Region before and after the Earthquake
There are a lot of landslides and debris flows developed in the Wenchuan earthquake region before the earthquake because of the wavy terrain,complex geological environment and rich rainfall.The Wenchuan earthquake triggered numerous landslides and debris flows.After the earthquake,not only landslides and debris flows become more active,but also the distribution of them has some new characteristics.Based on the distributions of landslides and debris flows before and after the earthquake,the characteristics of the distributions are analyzed and the quantitative regularity of their distribution after the earthquake is described.
Debris flow Landslide Wenchuan earthquake Distribution regularity Longmen Shan fault
WEI Fangqiang SU Pengcheng JIANG Yuhong
Key Laboratory of Mountain Hazards and Surface Process, Chinese Academy of Sciences, Chengdu 610041, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China
国际会议
成都
英文
16-26
2012-10-15(万方平台首次上网日期,不代表论文的发表时间)