Fluid-Rock Equilibria is a thermodynamic framework that describes the state of chemical equilibrium between coexisting rock-forming minerals and aqueous fluids under low-temperature conditions, accounting for the exchange of mass and energy to determine stable mineral assemblages and fluid compositions.
221
Publications
21.7K
Citations
821
Authors
334
Institutions
Publications per year
2017–2026
59
Publications
221
1–5 of 221
Authors
821
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5
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1–5 of 821
Institutions
334
Centre National de la Recherche Scientifique
Paris, France
9 h-index
26 publications
1.2K citations
ETH Zurich
Zurich, Switzerland
9 h-index
19 publications
1.2K citations
Chinese Academy of Sciences
Beijing, China
6 h-index
16 publications
335 citations
China University of Geosciences (Beijing)
Beijing, China
6 h-index
15 publications
606 citations
University of Alberta
Edmonton, Canada
5 h-index
14 publications
379 citations
University of Cambridge
Cambridge, United Kingdom
5 h-index
11 publications
10.3K citations
Los Alamos National Laboratory
Los Alamos, United States
5 h-index
12 publications
1.8K citations
China University of Petroleum, East China
Qingdao, China
4 h-index
14 publications
1.5K citations
1–8 of 334
Venues
- Geochimica et Cosmochimica Acta
19 publications · 1.8K citations
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- Contributions to Mineralogy and Petrology
14 publications · 1.3K citations
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- American Mineralogist
12 publications · 1.1K citations
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- Applied Geochemistry
9 publications · 272 citations
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- Economic Geology
9 publications · 599 citations
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