Hypocenter Migration
Hypocenter Migration is a spatiotemporal phenomenon in seismology characterized by the progressive displacement of earthquake hypocenters over time, distinguishing it from static source models by reflecting dynamic processes within the rupture zone such as fluid diffusion, stress transfer, or aseismic slip.
178
Publications
9.5K
Citations
661
Authors
195
Institutions
Publications per year
2017–2026
45
Parents
178
1–5 of 178
661
12
h-index
9
h-index
8
h-index
8
h-index
8
h-index
1–5 of 661
195

Tohoku University
Sendai, Japan
17 h-index
68 publications
2.8K citations
The University of Tokyo
Tokyo, Japan
16 h-index
59 publications
3.2K citations
United States Geological Survey
Reston, United States
14 h-index
38 publications
3.1K citations

Meteorological, Climatological, And Geophysical Agency
Jakarta, Indonesia
12 h-index
29 publications
890 citations
Bandung Institute of Technology
Bandung, Indonesia
12 h-index
57 publications
1.4K citations
Association for the Development of Earthquake Prediction
Tokyo, Japan
10 h-index
25 publications
2K citations

Kyoto University
Kyoto, Japan
8 h-index
33 publications
1.1K citations
National Research Institute for Earth Science and Disaster Resilience
Tsukuba, Japan
8 h-index
11 publications
519 citations
1–8 of 195
24 publications · 1K citations
20
h-index
BSSA · 26 publications · 1.1K citations
19
h-index
JGR · 19 publications · 1.9K citations
17
h-index
16 publications · 1.2K citations
16
h-index
10 publications · 413 citations
10
h-index
1–5