Finite-fault Source Effects
Finite-Fault Source Effects is a seismological construct that characterizes the spatial and temporal heterogeneity of rupture propagation across an extended fault plane during an earthquake, distinguishing it from point-source representations by accounting for variations in slip magnitude, timing, and direction over finite fault dimensions.
37
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6.5K
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104
Authors
46
Institutions
Publications per year
2017–2026
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California Institute of Technology
Pasadena, United States
5 h-index
6 publications
875 citations
ETH Zurich
Zurich, Switzerland
4 h-index
11 publications
835 citations
Stanford University
Stanford, United States
3 h-index
6 publications
1.5K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
3 h-index
4 publications
247 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
3 h-index
9 publications
462 citations
University of Science and Technology of China
Hefei, China
3 h-index
4 publications
171 citations

San Diego State University
San Diego, United States
3 h-index
6 publications
177 citations

Western University
London, Canada
2 h-index
3 publications
174 citations
1–8 of 46
BSSA · 14 publications · 4.8K citations
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5 publications · 281 citations
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GJI · 3 publications · 73 citations
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JGR · 3 publications · 217 citations
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SRL · 2 publications · 107 citations
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