Fluid-rock Equilibrium
Fluid-Rock Equilibrium is a geochemical state in which the mineral assemblages of a rock and the composition of an aqueous fluid phase coexist without net dissolution or precipitation, indicating thermodynamic equilibrium between the solid and fluid phases under specific temperature, pressure, and chemical potential conditions.
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2017–2026
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Fluid-rock interaction is decisive for the formation of tungsten deposits
Pilar Lecumberri–Sanchez, Romeu Vieira, Christoph A. Heinrich et al. · Geology · 2017 · 248 citations · Full text
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ETH Zurich
Zurich, Switzerland
6 h-index
8 publications
947 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
13 publications
520 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
5 h-index
13 publications
1.3K citations

University of Alberta
Edmonton, Canada
5 h-index
15 publications
441 citations

Sorbonne Université
Paris, France
4 h-index
7 publications
337 citations

University of Edinburgh
Edinburgh, United Kingdom
4 h-index
5 publications
256 citations
University of California, Los Angeles
Los Angeles, United States
4 h-index
4 publications
258 citations
Stanford University
Stanford, United States
4 h-index
7 publications
508 citations
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14 publications · 829 citations
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