Magma Ocean Solidification
Magma Ocean Solidification is a planetary-scale thermal evolution process denoting the gradual crystallization and differentiation of a global, molten silicate layer enveloping a nascent terrestrial planet, driven by conductive and convective heat loss, gravitational settling of dense minerals, and buoyant rise of light components, ultimately establishing the primordial mantle stratification and initiating crustal formation.
114
Publications
9.3K
Citations
340
Authors
190
Institutions
Publications per year
2017–2026
60
114
1–5 of 114
340
Massachusetts Institute of Technology, United States
12 publications · 2.4K citations
12
h-index
7
h-index
Centre National de la Recherche Scientifique, France
5 publications · 329 citations
5
h-index
5
h-index
4
h-index
1–5 of 340
190

Centre National de la Recherche Scientifique
Paris, France
17 h-index
45 publications
4.1K citations

Carnegie Institution for Science
Washington, United States
11 h-index
11 publications
1.1K citations
Brown University
Providence, United States
10 h-index
26 publications
2.1K citations

Institut de physique du globe de Paris
Paris, France
9 h-index
19 publications
1.9K citations
ETH Zurich
Zurich, Switzerland
9 h-index
15 publications
1.1K citations
Massachusetts Institute of Technology
Cambridge, United States
9 h-index
13 publications
2.5K citations
Planetary Science Institute
Tucson, United States
9 h-index
16 publications
1.5K citations

Vrije Universiteit Amsterdam
Amsterdam, The Netherlands
8 h-index
19 publications
1.7K citations
1–8 of 190
13 publications · 1.8K citations
13
h-index
10 publications · 444 citations
10
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8 publications · 514 citations
8
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6 publications · 310 citations
6
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5 publications · 240 citations
5
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1–5