Time-dependent Fault Strength
Time-Dependent Fault Strength is a geomechanical property representing the progressive evolution of a fault's resistance to shear failure over time due to post-seismic healing, creep, and interseismic stress accumulation, distinguishing it from instantaneous or static measures of fault strength by explicitly incorporating temporal variations in frictional and cohesive behavior along fault zones.
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James F. Dolan, Lee J. McAuliffe, Edward J. Rhodes et al. · Earth and Planetary Science Letters · 2016 · 100 citations
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Utrecht University
Utrecht, The Netherlands
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5 publications
126 citations
Institut de Recherche pour le Développement
Marseille, France
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2 publications
53 citations
University of Oklahoma
Norman, United States
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2 publications
153 citations
Planetary Science Institute
Tucson, United States
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3 publications
144 citations
Observatoire de la Côte d’Azur
Nice, France
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2 publications
53 citations
University of Bremen
Bremen, Germany
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4 publications
195 citations
University of Southern California
Los Angeles, United States
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5 publications
796 citations
The University of Tokyo
Tokyo, Japan
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2 publications
85 citations
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JGR · 3 publications · 201 citations
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PAGEOPH · 2 publications · 265 citations
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