Fault Segment Interaction
Fault Segment Interaction is a geomechanical process denoting the stress-mediated influence between adjacent or nearby segments of a fault system during and after an earthquake, where the rupture dynamics and post-seismic deformation of one segment alter the mechanical state and rupture potential of neighboring segments.
93
Publications
6.4K
Citations
269
Authors
148
Institutions
Publications per year
2017–2026
13
Parents
93
Joseph A. Cartwright, Bruce D. Trudgill, Christopher S. Mansfield · Journal of Structural Geology · 1995 · 691 citations
1–5 of 93
269
3
h-index
3
h-index
2
h-index
2
h-index
2
h-index
1–5 of 269
148

Centre National de la Recherche Scientifique
Paris, France
7 h-index
17 publications
1.1K citations
United States Geological Survey
Reston, United States
6 h-index
13 publications
547 citations
Stanford University
Stanford, United States
4 h-index
8 publications
1K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
4 h-index
12 publications
539 citations
University of California, Santa Cruz
Santa Cruz, United States
4 h-index
6 publications
209 citations

Imperial College London
London, United Kingdom
4 h-index
10 publications
2.3K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
11 publications
921 citations

Institut de physique du globe de Paris
Paris, France
4 h-index
10 publications
591 citations
1–8 of 148
10 publications · 2.4K citations
10
h-index
JGR · 10 publications · 746 citations
10
h-index
6 publications · 201 citations
6
h-index
5 publications · 824 citations
5
h-index
4 publications · 182 citations
4
h-index
1–5