Mantle Phase Equilibria
Mantle Phase Equilibria is a thermodynamic framework that describes the stable mineralogical assemblages and their equilibrium conditions under varying pressure, temperature, and bulk composition within Earth's mantle.
612
Publications
50.5K
Citations
1.2K
Authors
400
Institutions
Publications per year
2017–2026
108
Parents
612
1–5 of 612
1.2K
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400
University of Bayreuth
Bayreuth, Germany
27 h-index
92 publications
5.4K citations
Tokyo Institute of Technology
Tokyo, Japan
23 h-index
50 publications
5.2K citations

Carnegie Institution for Science
Washington, United States
22 h-index
50 publications
8.1K citations
Japan Synchrotron Radiation Research Institute
Sayō, Japan
21 h-index
39 publications
3K citations

Tohoku University
Sendai, Japan
21 h-index
58 publications
4.8K citations
ETH Zurich
Zurich, Switzerland
21 h-index
38 publications
3.2K citations
Ehime University
Matsuyama, Japan
21 h-index
67 publications
3.5K citations
California Institute of Technology
Pasadena, United States
20 h-index
34 publications
4.3K citations
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80 publications · 7K citations
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JGR · 55 publications · 5.9K citations
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56 publications · 3.8K citations
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50 publications · 3.8K citations
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43 publications · 2.3K citations
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