Mantle Downwelling
Mantle Downwelling is a large-scale geodynamical process within mantle convection characterized by the sinking of cooler, denser mantle material from the upper mantle toward the core-mantle boundary, driven by gravitational instability and plate tectonic forces.
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2017–2026
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Variants
Mantle Downwellings
Parents
71
Dehydration melting at the top of the lower mantle
Brandon Schmandt, Steven D. Jacobsen, T. W. Becker et al. · Science · 2014 · 355 citations
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California Institute of Technology
Pasadena, United States
6 h-index
11 publications
1.2K citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
7 publications
676 citations
Los Alamos National Laboratory
Los Alamos, United States
4 h-index
6 publications
900 citations
University of California, Los Angeles
Los Angeles, United States
3 h-index
4 publications
213 citations
Arizona State University
Tempe, United States
3 h-index
5 publications
318 citations

Carnegie Institution for Science
Washington, United States
3 h-index
3 publications
472 citations
Planetary Science Institute
Tucson, United States
3 h-index
6 publications
846 citations

University of Leeds
Leeds, United Kingdom
3 h-index
3 publications
168 citations
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16 publications · 725 citations
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JGR · 9 publications · 917 citations
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GJI · 8 publications · 438 citations
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7 publications · 739 citations
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6 publications · 1.1K citations
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