Fault Healing
Fault healing is a mechanical process in which the strength and cohesion of a fault zone are progressively restored over time following an earthquake, primarily through time-dependent rock deformation mechanisms such as asperity creep, mineral precipitation, and pore sealing under in-situ pressure and temperature conditions.
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8.1K
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203
Authors
119
Institutions
Publications per year
2017–2026
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Utrecht University
Utrecht, The Netherlands
8 h-index
21 publications
1.5K citations

Pennsylvania State University
State College, United States
6 h-index
15 publications
1.1K citations
Massachusetts Institute of Technology
Cambridge, United States
6 h-index
9 publications
3.4K citations
Planetary Science Institute
Tucson, United States
4 h-index
6 publications
497 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
3 h-index
5 publications
576 citations
Princeton University
Princeton, United States
3 h-index
6 publications
1.5K citations
The University of Tokyo
Tokyo, Japan
3 h-index
3 publications
225 citations
Columbia University
New York, United States
3 h-index
5 publications
576 citations
1–8 of 119
JGR · 11 publications · 1.6K citations
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10 publications · 329 citations
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6 publications · 434 citations
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BSSA · 4 publications · 346 citations
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GJI · 3 publications · 97 citations
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