Core-mantle Partitioning
Core-Mantle Partitioning is a geochemical process that describes the distribution of elements between the Earth's metallic core and silicate mantle during planetary differentiation, distinguished by the affinity of elements to metal versus silicate phases under high-pressure and high-temperature conditions.
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182
Institutions
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2017–2026
38
Variants
Core-mantle Element Partitioning
Parents
159
Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity
James Badro, G. Fiquet, François Guyot et al. · Science · 2003 · 523 citations
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University of Bayreuth
Bayreuth, Germany
16 h-index
46 publications
4.2K citations

Carnegie Institution for Science
Washington, United States
13 h-index
30 publications
5.5K citations

Centre National de la Recherche Scientifique
Paris, France
13 h-index
39 publications
5.9K citations
Planetary Science Institute
Tucson, United States
10 h-index
18 publications
1.8K citations

Institut de physique du globe de Paris
Paris, France
10 h-index
34 publications
2.4K citations
Université Paris Cité
Paris, France
9 h-index
36 publications
5.7K citations
Tokyo Institute of Technology
Tokyo, Japan
9 h-index
14 publications
860 citations
Geophysical Laboratory
Washington, United States
8 h-index
23 publications
4.8K citations
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21 publications · 1.9K citations
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18 publications · 1.5K citations
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18 publications · 877 citations
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10 publications · 2.1K citations
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9 publications · 736 citations
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