【摘 要】
：
In the Wenchuan area in SW China, an abundance of loose co-seismic landslide debris was present on the slopes after the Wenchuan earthquake, which in later years served as source material for rainfall
【机 构】
：
State Key Laboratory of Geo-Hazard Prevention and Geo-Environment Protection,Chengdu University of T
【出 处】
：
The International Symposium and 9th Asian Regional Conferenc
论文部分内容阅读
In the Wenchuan area in SW China, an abundance of loose co-seismic landslide debris was present on the slopes after the Wenchuan earthquake, which in later years served as source material for rainfall-induced debris flows or shallow landslides.
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