Fault Slip Instability is a geomechanical phenomenon characterized by the sudden and self-sustaining failure of a fault plane under stress, distinguished from stable slip by its propensity to accelerate into seismic rupture due to rate-dependent frictional weakening.
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Utrecht University
Utrecht, The Netherlands
7 h-index
15 publications
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China Earthquake Administration
Beijing, China
5 h-index
15 publications
318 citations
Pennsylvania State University
State College, United States
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381 citations
United States Geological Survey
Reston, United States
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10 publications
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University of Southern California
Los Angeles, United States
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Institute of Geology, China Earthquake Administration
Beijing, China
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Southern California Earthquake Center
Los Angeles, United States
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Université Savoie Mont Blanc
Chambéry, France
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57 citations
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- Tectonophysics
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- Journal of Geophysical Research Solid Earth
7 publications · 212 citations
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PAGEOPH · 6 publications · 469 citations
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