Fault Strength Evolution
Fault Strength Evolution is the time-dependent process by which the mechanical resistance of a fault to shear slip changes due to variations in stress, frictional properties, fluid pressure, and rock damage, distinguishing it from static fault strength models by explicitly accounting for dynamic physicochemical feedbacks during the earthquake nucleation cycle.
175
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14K
Citations
479
Authors
213
Institutions
Publications per year
2017–2026
41
175
On the relation between fault strength and frictional stability
Matt J. Ikari, Chris Marone, D. M. Saffer · Geology · 2010 · 370 citations
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479
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Japan Agency for Marine-Earth Science and Technology, Japan
4 publications · 269 citations
4
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4
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213

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
11 h-index
29 publications
2K citations
United States Geological Survey
Reston, United States
11 h-index
28 publications
3.3K citations
Utrecht University
Utrecht, The Netherlands
7 h-index
12 publications
1K citations

Pennsylvania State University
State College, United States
7 h-index
20 publications
2.4K citations
University of Oklahoma
Norman, United States
6 h-index
10 publications
450 citations
University of Southern California
Los Angeles, United States
6 h-index
10 publications
979 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
7 publications
691 citations
Curtin University
Perth, Australia
5 h-index
5 publications
208 citations
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20 publications · 1.9K citations
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15 publications · 1.1K citations
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JGR · 14 publications · 2.5K citations
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15 publications · 585 citations
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13 publications · 1.6K citations
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