Mantle Fractionation
Mantle Fractionation is a geochemical process within planetary differentiation whereby successive melting and extraction of material from the Earth's mantle generate compositionally distinct rock types, distinguished by the preferential removal of specific minerals or elements during partial melting events.
430
Publications
64.1K
Citations
1.4K
Authors
456
Institutions
Publications per year
2017–2026
83
Parents
430
1.4K
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456

Centre National de la Recherche Scientifique
Paris, France
25 h-index
76 publications
10K citations

Chinese Academy of Sciences
Beijing, China
21 h-index
96 publications
4.7K citations

Carnegie Institution for Science
Washington, United States
17 h-index
34 publications
6.2K citations

Institut de physique du globe de Paris
Paris, France
15 h-index
30 publications
2.6K citations

Macquarie University
Sydney, Australia
14 h-index
30 publications
3.8K citations
Guangzhou Institute of Geochemistry
Guangzhou, China
13 h-index
38 publications
2.8K citations
University of Bayreuth
Bayreuth, Germany
13 h-index
32 publications
2.4K citations

China University of Geosciences (Beijing)
Beijing, China
13 h-index
31 publications
2.3K citations
1–8 of 456
52 publications · 3.7K citations
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36 publications · 6K citations
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26 publications · 2.7K citations
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JGR · 23 publications · 3.8K citations
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19 publications · 1.4K citations
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