Mineral Equilibrium
Mineral Equilibrium is a theoretical state within mineral paragenesis denoting the condition in which the assemblage of coexisting minerals in a rock system remains stable over time, with no net change in mineral composition or phase distribution under constant physical and chemical conditions.
121
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8K
Citations
257
Authors
140
Institutions
Publications per year
2017–2026
19
Parents
121
Gordon Moore, I. S. E. Carmichael · Contributions to Mineralogy and Petrology · 1998 · 478 citations
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University of Tsukuba
Tsukuba, Japan
10 h-index
20 publications
493 citations

University of Johannesburg
Johannesburg, South Africa
8 h-index
8 publications
183 citations

The University of Melbourne
Melbourne, Australia
6 h-index
13 publications
689 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
9 publications
398 citations

China University of Geosciences (Beijing)
Beijing, China
5 h-index
5 publications
131 citations
United States Geological Survey
Reston, United States
5 h-index
6 publications
106 citations
University of California, Berkeley
Berkeley, United States
4 h-index
8 publications
1.3K citations
University of Cambridge
Cambridge, United Kingdom
4 h-index
4 publications
236 citations
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14 publications · 763 citations
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12 publications · 1.2K citations
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10 publications · 880 citations
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7 publications · 799 citations
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5 publications · 308 citations
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