Mantle Upwelling
Mantle Upwelling is a geophysical process in which buoyant, thermally activated mantle material rises from deeper regions of the Earth's interior toward the surface, driven by thermal convection and decompression melting, particularly beneath divergent plate boundaries such as mid-ocean ridges and continental rift zones.
327
Publications
24K
Citations
914
Authors
379
Institutions
Publications per year
2017–2026
74
327
Seismic Evidence for Partial Melt at the Base of Earth's Mantle
Quentin Williams, Edward J. Garnero · Science · 1996 · 587 citations
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Missouri University of Science and Technology, United States
5 publications · 118 citations
5
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5
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379

Centre National de la Recherche Scientifique
Paris, France
18 h-index
62 publications
4.3K citations

Chinese Academy of Sciences
Beijing, China
15 h-index
48 publications
2.3K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
15 h-index
25 publications
1.7K citations
China Earthquake Administration
Beijing, China
13 h-index
23 publications
931 citations
Columbia University
New York, United States
13 h-index
21 publications
1.4K citations
Woods Hole Oceanographic Institution
Falmouth, United States
13 h-index
19 publications
3.6K citations

Tohoku University
Sendai, Japan
12 h-index
22 publications
1.4K citations
Brown University
Providence, United States
12 h-index
28 publications
1.7K citations
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JGR · 37 publications · 4.2K citations
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35 publications · 1.7K citations
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26 publications · 1.9K citations
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20 publications · 1.2K citations
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GJI · 20 publications · 1.2K citations
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