Core Mantle Structure
Core Mantle Structure is a planetary differentiation model that specifies the concentric stratification of a terrestrial planet into a dense metallic core and a overlying silicate mantle, distinguished by differences in composition, density, and rheological behavior resulting from gravitational separation during planetary accretion and igneous processes.
296
Publications
22.7K
Citations
658
Authors
298
Institutions
Publications per year
2017–2026
32
Variants
Core-mantle Structure
Parents
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Planetary Science Institute
Tucson, United States
20 h-index
41 publications
3.8K citations
California Institute of Technology
Pasadena, United States
19 h-index
35 publications
3K citations

Centre National de la Recherche Scientifique
Paris, France
15 h-index
45 publications
3.5K citations
Massachusetts Institute of Technology
Cambridge, United States
13 h-index
30 publications
2.2K citations

Institut de physique du globe de Paris
Paris, France
12 h-index
30 publications
3.9K citations
University of California, Santa Cruz
Santa Cruz, United States
11 h-index
15 publications
1.6K citations

Carnegie Institution for Science
Washington, United States
11 h-index
20 publications
1.4K citations
Harvard University
Cambridge, United States
10 h-index
15 publications
2.1K citations
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JGR · 27 publications · 3.1K citations
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32 publications · 2.1K citations
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26 publications · 2.9K citations
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GJI · 31 publications · 2.1K citations
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24 publications · 1.2K citations
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