Permanent Ground Strain
Permanent Ground Strain is a geophysical phenomenon denoting the irreversible deformation of the Earth's crust along a fault zone, persisting after the passage of seismic waves during an earthquake, thereby representing the final, non-recoverable displacement field recorded in the solid earth.
24
Publications
847
Citations
66
Authors
45
Institutions
Publications per year
2017–2026
7
Variants
Coseismic Strain
Parents
24
1–5 of 24
66
5
h-index
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1–5 of 66
45
Rensselaer Polytechnic Institute
Troy, United States
5 h-index
8 publications
175 citations
Tokyo University of Science
Tokyo, Japan
2 h-index
3 publications
80 citations

Advanced Institute of Industrial Technology
Tokyo, Japan
2 h-index
3 publications
80 citations
National Technical University of Athens
Athens, Greece
2 h-index
3 publications
51 citations
University of Illinois Urbana-Champaign
Urbana, United States
2 h-index
2 publications
46 citations
United States Geological Survey
Reston, United States
2 h-index
2 publications
119 citations
University of California, Berkeley
Berkeley, United States
1 h-index
1 publications
17 citations
Bu-Ali Sina University
Hamadan, Iran
1 h-index
2 publications
86 citations
1–8 of 45
3 publications · 53 citations
3
h-index
2 publications · 74 citations
2
h-index
1 publications · 25 citations
2
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2 publications · 144 citations
2
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1 publications · 24 citations
1
h-index
1–5