Subduction-Driven Mantle Flow is a geodynamic model of mantle convection in which the primary mechanistic driver is the sinking of dense oceanic lithosphere into the mantle at subduction zones, distinguishing it from models dominated by bottom-up buoyancy or passive flow mechanisms.
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485
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Publications per year
2017–2026
128
Parents
Publications
510
Robert J. Stern · Reviews of Geophysics · 2002 · 1.4K citations
Deep Mantle Convection Plumes and Plate Motions
W. Jason Morgan · AAPG Bulletin · 1972 · 936 citations
Trench-Parallel Flow Beneath the Nazca Plate from Seismic Anisotropy
R. M. Russo, Paul G. Silver · Science · 1994 · 513 citations
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Centre National de la Recherche Scientifique
Paris, France
28 h-index
91 publications
5.9K citations
Monash University
Melbourne, Australia
25 h-index
49 publications
3.3K citations
Planetary Science Institute
Tucson, United States
24 h-index
42 publications
3.5K citations
California Institute of Technology
Pasadena, United States
20 h-index
38 publications
4.4K citations
Australian National University
Canberra, Australia
19 h-index
31 publications
3.8K citations
Chinese Academy of Sciences
Beijing, China
17 h-index
52 publications
2.1K citations
Roma Tre University
Rome, Italy
16 h-index
37 publications
3.1K citations
Yale University
New Haven, United States
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30 publications
2.5K citations
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- Earth and Planetary Science Letters
79 publications · 7K citations
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- Journal of Geophysical Research Atmospheres
JGR · 43 publications · 5.8K citations
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- Geophysical Research Letters
47 publications · 3.2K citations
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- Geology
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- Geochemistry Geophysics Geosystems
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