Foreshock Migration
Foreshock Migration is a seismic phenomenon in seismology characterized by the spatial and temporal progression of foreshock activity toward the eventual mainshock hypocenter, distinguishing it from random or static foreshock clustering.
23
Publications
1.1K
Citations
90
Authors
47
Institutions
Publications per year
2017–2026
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90
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Tohoku University
Sendai, Japan
4 h-index
11 publications
1.2K citations
China Earthquake Administration
Beijing, China
3 h-index
9 publications
206 citations
The University of Tokyo
Tokyo, Japan
2 h-index
5 publications
515 citations
Geological Survey of Japan
Tsukuba, Japan
2 h-index
4 publications
216 citations
National Observatory of Athens
Athens, Greece
2 h-index
2 publications
39 citations
University of Southern California
Los Angeles, United States
2 h-index
2 publications
96 citations
University of California, Berkeley
Berkeley, United States
2 h-index
4 publications
152 citations
Planetary Science Institute
Tucson, United States
2 h-index
5 publications
265 citations
1–8 of 47
5 publications · 476 citations
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BSSA · 3 publications · 103 citations
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2 publications · 85 citations
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2 publications · 83 citations
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1 publications · 11 citations
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1–5