Intermediate-depth Seismicity
Intermediate-Depth Seismicity is a class of intraplate earthquakes occurring at depths between 70 and 300 kilometers, distinguished from shallow and deep seismicity by its association with metamorphic dehydration reactions and slab-derived processes within subducting lithospheric plates.
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22.5K
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Authors
338
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2017–2026
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Bradley R. Hacker, Simon M. Peacock, G. A. Abers et al. · Journal of Geophysical Research Atmospheres · 2003 · 1K citations · Full text
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Institutul National de Cercetare si Dezvoltare pentru Fizica Pamantului, Romania
16 publications · 641 citations
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Technical University of Civil Engineering of Bucharest, Romania
8 publications · 165 citations
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Centre National de la Recherche Scientifique
Paris, France
19 h-index
72 publications
3.8K citations
Institutul National de Cercetare si Dezvoltare pentru Fizica Pamantului
Măgurele, Romania
16 h-index
47 publications
1.5K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
15 h-index
38 publications
2.8K citations

Tohoku University
Sendai, Japan
13 h-index
36 publications
1.3K citations
Massachusetts Institute of Technology
Cambridge, United States
12 h-index
28 publications
1.6K citations

Kyoto University
Kyoto, Japan
11 h-index
18 publications
786 citations
University of Chile
Santiago, Chile
11 h-index
38 publications
1.4K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
10 h-index
16 publications
1.3K citations
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JGR · 50 publications · 4.7K citations
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GJI · 41 publications · 3.7K citations
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BSSA · 27 publications · 1.8K citations
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