A study of the pro-water pressure for initiation of a large landslide triggered by a strong earthquake based on fluid-structure coupling

The Daguangbao landslide is the largest co-seismic landslide with a volume of approximately 12×108 m3, which triggered by the Wenchuan earthquake (Ms 8.0) occurred on May 12, 2008. The slide zone is located in the Paleozoic carbonate strata and it is an interlayer structural dislocation zone with a...

Full description

Bibliographic Details

Published in:	Shuiwen dizhi gongcheng dizhi
Main Authors:	Xingxing SHI, Shenghua CUI, Xiangjun PEI, Ling ZHU, Qingwen YANG
Format:	Article
Language:	Chinese
Published:	Editorial Office of Hydrogeology & Engineering Geology 2022-03-01
Subjects:	wenchuan earthquake daguangbao landslide groundwater excess pore water pressure fluid-structure coupling flac3d
Online Access:	https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202104052