Reactivation mechanism and run-out processes of the Wangqi landslide induced by water leakage on April 30, 2022, in Tianshui City, Gansu Province, China

Author:

Wang Haojie,Sun Ping,Ren Jian,Mao Jiarui,Ke Chaoying

Funder

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

Geotechnical Engineering and Engineering Geology

Reference28 articles.

1. Bhambri R, Mehta M, Singh S, Perumal RJ, Srivastava P (2017) Landslide inventory and damage assessment in the Bhagirathi Valley, Uttarakhand, during June 2013 flood. Himalayan Geol 38:193–205

2. Chen P, Lin A (2019) Tectonic topography and late Pleistocene activity of the West Qinling fault, Northeastern Tibetan Plateau. J Asian Earth Sci 176:68–78. https://doi.org/10.1016/j.jseaes.2019.02.007

3. Fan X, Xu Q, Zhang Z, Meng D, Tang R (2009) The genetic mechanism of a translational landslide. Bull Eng Geol Env 68:231–244. https://doi.org/10.1007/s10064-009-0194-1

4. Glastonbury J, Fell R (2008) Geotechnical characteristics of large slow, very slow, and extremely slow landslides. Can Geotech J 45:984–1005. https://doi.org/10.1139/T08-021

5. Guo C, Wang T, Sun P (2020) Report of secondary project of engineering geological survey of Tianshui and other towns and Chengdu-Lanzhou Traffic Corridor in Gansu Province [DS]. China Geological Survey

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