Fault Rupture Dynamics is a theoretical framework within earthquake source physics that characterizes the temporally and spatially evolving processes of mechanical failure, slip propagation, and stress transfer along a fault interface during seismic rupture.
572
Publications
43.3K
Citations
1.4K
Authors
448
Institutions
Publications per year
2017–2026
167
Publications
572
1–5 of 572
Authors
1.4K
- DD
20
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- JA
17
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- AG
13
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- TU
12
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1–5 of 1.4K
Institutions
448
California Institute of Technology
Pasadena, United States
33 h-index
92 publications
9.3K citations
United States Geological Survey
Reston, United States
31 h-index
64 publications
6.2K citations
China Earthquake Administration
Beijing, China
24 h-index
94 publications
12K citations
San Diego State University
San Diego, United States
22 h-index
43 publications
3K citations
Centre National de la Recherche Scientifique
Paris, France
21 h-index
55 publications
4.9K citations
Scripps Institution of Oceanography
La Jolla, United States
20 h-index
38 publications
3.3K citations
University of California San Diego
San Diego, United States
19 h-index
39 publications
3.3K citations
Planetary Science Institute
Tucson, United States
18 h-index
35 publications
5K citations
1–8 of 448
Venues
- Bulletin of the Seismological Society of America
BSSA · 66 publications · 5.8K citations
38
h-index
- Journal of Geophysical Research Atmospheres
JGR · 50 publications · 6.3K citations
36
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- Geophysical Research Letters
53 publications · 2.9K citations
29
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- Journal of Geophysical Research Solid Earth
38 publications · 2.5K citations
28
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- Tectonophysics
34 publications · 2.7K citations
26
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