Double Seismic Zone
A "Double Seismic Zone" is a distinct seismic structure within a subducting slab characterized by two parallel planes of earthquake hypocenters, distinguished from other intraslab seismic patterns by their consistent separation and orientation, typically interpreted as resulting from phase transformations and stress variations in the downgoing lithosphere.
95
Publications
6.4K
Citations
244
Authors
125
Institutions
Publications per year
2017–2026
17
Variants
Double Benioff Zone
Parents
95
1–5 of 95
244
10
h-index
6
h-index
5
h-index
5
h-index
5
h-index
1–5 of 244
125

Tohoku University
Sendai, Japan
16 h-index
53 publications
5.3K citations
The University of Tokyo
Tokyo, Japan
8 h-index
14 publications
1.3K citations
University of Chile
Santiago, Chile
6 h-index
11 publications
637 citations
National Research Institute for Earth Science and Disaster Resilience
Tsukuba, Japan
6 h-index
7 publications
150 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
18 publications
1.1K citations
Association for the Development of Earthquake Prediction
Tokyo, Japan
5 h-index
15 publications
1.6K citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
7 publications
163 citations
Columbia University
New York, United States
5 h-index
7 publications
696 citations
1–8 of 125
JGR · 20 publications · 1.8K citations
19
h-index
20 publications · 923 citations
16
h-index
GJI · 11 publications · 795 citations
11
h-index
7 publications · 691 citations
7
h-index
4 publications · 191 citations
4
h-index
1–5