Flow Slides
Flow Slide is a type of slope failure mechanism characterized by the rapid, fluid-like deformation and downslope movement of saturated, fine-grained soils or weak rock masses, distinguished from other slope failures by its low resistance to shear stress and continuous, viscous flow behavior.
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3.1K
Citations
165
Authors
72
Institutions
Publications per year
2017–2026
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Tongji University
Shanghai, China
5 h-index
13 publications
403 citations
Chang'an University
Xi'an, China
3 h-index
7 publications
466 citations
Politecnico di Milano
Milan, Italy
3 h-index
3 publications
143 citations

Delft University of Technology
Delft, The Netherlands
3 h-index
10 publications
151 citations
China Earthquake Administration
Beijing, China
2 h-index
2 publications
33 citations

University of British Columbia
Vancouver, Canada
2 h-index
2 publications
110 citations
Deltares
Delft, The Netherlands
2 h-index
2 publications
45 citations
University of Washington
Seattle, United States
2 h-index
3 publications
81 citations
1–8 of 72
13 publications · 719 citations
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4 publications · 355 citations
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4 publications · 114 citations
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3 publications · 46 citations
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2 publications · 128 citations
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