Mantle Circulation
Mantle Circulation is a geophysical process denoting the large-scale movement of material within Earth's mantle driven by thermal convection, distinguished from other forms of mantle dynamics by its primary role in facilitating heat transfer and plate tectonic motion through viscous flow over geological timescales.
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2017–2026
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Evidence for deep mantle circulation from global tomography
Robert D. van der Hilst, Sri Widiyantoro, E. R. Engdahl · Nature · 1997 · 1.3K citations · Full text
Finite deformation during fluid flow
Dan McKenzie · Geophysical Journal International · 1979 · 396 citations
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Centre National de la Recherche Scientifique
Paris, France
15 h-index
35 publications
1.9K citations
Los Alamos National Laboratory
Los Alamos, United States
10 h-index
12 publications
2.2K citations
California Institute of Technology
Pasadena, United States
10 h-index
12 publications
822 citations

University of Minnesota
Minneapolis, United States
10 h-index
16 publications
1.5K citations
Planetary Science Institute
Tucson, United States
9 h-index
13 publications
1.3K citations

University of Toronto
Toronto, Canada
9 h-index
11 publications
886 citations

Johns Hopkins University
Baltimore, United States
8 h-index
13 publications
991 citations
Ludwig-Maximilians-Universität München
Munich, Germany
8 h-index
22 publications
1.9K citations
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JGR · 29 publications · 3.2K citations
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27 publications · 2.5K citations
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20 publications · 1.8K citations
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18 publications · 883 citations
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19 publications · 3.5K citations
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