Intermediate-depth Earthquakes
Intermediate-Depth Earthquakes is a class of tectonic seismic events occurring within subducting lithospheric plates at depths between 70 and 300 kilometers, distinguished from shallow and deep earthquakes by their specific depth range and association with dehydration embrittlement and phase transformations in the mantle.
379
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25.4K
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860
Authors
320
Institutions
Publications per year
2017–2026
73
Parents
379
Bradley R. Hacker, Simon M. Peacock, G. A. Abers et al. · Journal of Geophysical Research Atmospheres · 2003 · 1K citations · Full text
High-Pressure Creep of Serpentine, Interseismic Deformation, and Initiation of Subduction
Nadège Hilairet, Bruno Reynard, Yanbin Wang et al. · Science · 2007 · 433 citations
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Institutul National de Cercetare si Dezvoltare pentru Fizica Pamantului, Romania
16 publications · 604 citations
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Centre National de la Recherche Scientifique
Paris, France
19 h-index
76 publications
6.8K citations
Institutul National de Cercetare si Dezvoltare pentru Fizica Pamantului
Măgurele, Romania
16 h-index
57 publications
1.6K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
16 h-index
37 publications
2.6K citations

Tohoku University
Sendai, Japan
14 h-index
40 publications
1.5K citations

Kyoto University
Kyoto, Japan
14 h-index
23 publications
910 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
13 h-index
17 publications
1.2K citations
Aristotle University of Thessaloniki
Thessaloniki, Greece
12 h-index
30 publications
1K citations
Columbia University
New York, United States
11 h-index
15 publications
1.1K citations
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JGR · 63 publications · 7K citations
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GJI · 42 publications · 4K citations
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39 publications · 1.7K citations
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BSSA · 32 publications · 2K citations
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14 publications · 695 citations
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