Faulting Mechanisms
Faulting Mechanisms is a seismological construct that characterizes the specific processes and physical conditions governing the formation and movement of fractures in planetary lithospheres due to stress accumulation and release.
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689
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2017–2026
106
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746
The seismogenic zone of subduction thrust faults
R. D. Hyndman, Makoto Yamano, D. A. Oleskevich · Island Arc · 1997 · 627 citations
Central role of detachment faults in accretion of slow-spreading oceanic lithosphere
J. Escartı́n, Deborah K. Smith, J. Cann et al. · Nature · 2008 · 505 citations
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United States Geological Survey
Reston, United States
26 h-index
67 publications
4.7K citations
Planetary Science Institute
Tucson, United States
23 h-index
49 publications
5.6K citations

Centre National de la Recherche Scientifique
Paris, France
22 h-index
79 publications
3.9K citations
California Institute of Technology
Pasadena, United States
19 h-index
34 publications
1.9K citations
ETH Zurich
Zurich, Switzerland
17 h-index
49 publications
2.5K citations

Institut de physique du globe de Paris
Paris, France
16 h-index
47 publications
4.4K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
16 h-index
27 publications
2.2K citations
University of Cambridge
Cambridge, United Kingdom
15 h-index
22 publications
1.9K citations
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JGR · 63 publications · 5.3K citations
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60 publications · 5.1K citations
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