Initiation, movement, and run-out of the giant Tsaoling landslide — What can we learn from a simple rigid block model and a velocity–displacement dependent friction law?-Reference-Cited by-同舟云学术

Initiation, movement, and run-out of the giant Tsaoling landslide — What can we learn from a simple rigid block model and a velocity–displacement dependent friction law?

Published:2014-11 Issue: Volume:182 Page:158-181
ISSN:0013-7952
Container-title:Engineering Geology
language:en
Short-container-title:Engineering Geology

Author:

Yang Che-Ming,Yu Wei-Lun,Dong Jia-Jyun,Kuo Chih-Yu,Shimamoto Toshihiko,Lee Chyi-Tyi,Togo Tetsuhiro,Miyamoto Yuki

Funder

National Science Council, Taiwan

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology

Reference81 articles.

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4. Clay clast aggregates in gouges: new textural evidence for seismic faulting;Boutareaud;J. Geophys. Res.,2010

5. Friction of rocks;Byerlee;Pure Appl. Geophys.,1978

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