Core-mantle Equilibrium
Core-Mantle Equilibrium is a geochemical model that describes the state of chemical and isotopic partitioning between Earth's metallic core and silicate mantle achieved through high-pressure, high-temperature equilibration during planetary differentiation.
444
Publications
35.9K
Citations
940
Authors
353
Institutions
Publications per year
2017–2026
75
Parents
444
Melting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray Diffraction
Simone Anzellini, Agnès Dewaele, Mohamed Mézouar et al. · Science · 2013 · 615 citations · Full text
D. J. Stevenson · Science · 1981 · 479 citations
Evolution of Planetary Cores and the Earth-Moon System from Nb/Ta Systematics
Carsten Münker, Jörg A. Pfänder, Stefan Weyer et al. · Science · 2003 · 451 citations
1–5 of 444
940
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V.S. Sobolev Institute of Geology and Mineralogy, Russia
9 publications · 316 citations
9
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9
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9
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1–5 of 940
353
Planetary Science Institute
Tucson, United States
27 h-index
57 publications
5.9K citations

Centre National de la Recherche Scientifique
Paris, France
26 h-index
98 publications
6.9K citations
University of California, Berkeley
Berkeley, United States
21 h-index
39 publications
5.2K citations

Carnegie Institution for Science
Washington, United States
21 h-index
58 publications
5.9K citations
University of Bayreuth
Bayreuth, Germany
20 h-index
51 publications
5.4K citations

Institut de physique du globe de Paris
Paris, France
19 h-index
54 publications
3.8K citations
Tokyo Institute of Technology
Tokyo, Japan
16 h-index
37 publications
5.1K citations

University of Minnesota
Minneapolis, United States
15 h-index
35 publications
4.5K citations
1–8 of 353
71 publications · 6.1K citations
41
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57 publications · 3.7K citations
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41 publications · 2.4K citations
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27 publications · 4.3K citations
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25 publications · 2K citations
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