Aqueous Fluid-Silicate Interaction is a geochemical process involving the chemical exchange and reaction between aqueous fluids and silicate minerals under high-temperature conditions, distinguishing it from low-temperature alteration processes by its characteristic thermodynamic stability fields, enhanced ion mobility, and role in magmatic and metamorphic fluid-rock interaction.
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Silica diagenesis; II, General mechanisms
L. A. Williams, David A. Crerar · Journal of Sedimentary Research · 1985 · 369 citations
Roland Hellmann, Richard Wirth, Damien Daval et al. · Chemical Geology · 2011 · 314 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
16 h-index
57 publications
3.7K citations
Carnegie Institution for Science
Washington, United States
9 h-index
11 publications
303 citations
University of California, Berkeley
Berkeley, United States
8 h-index
16 publications
1.2K citations
Chinese Academy of Sciences
Beijing, China
6 h-index
18 publications
760 citations
Geophysical Laboratory
Washington, United States
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6 publications
165 citations
Eindhoven University of Technology
Eindhoven, The Netherlands
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24 publications
596 citations
University of Maryland, College Park
College Park, United States
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GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
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- Chemical Geology
11 publications · 1K citations
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- American Mineralogist
10 publications · 407 citations
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- Earth and Planetary Science Letters
9 publications · 660 citations
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