Fluid Source Constraints
Fluid Source Constraints is a geochemical construct that specifies the permissible origins and compositional limits of hydrothermal fluids responsible for metasomatic alteration and mineralization in skarn systems, differentiating it from broader fluid-related models by focusing on isotopic, elemental, and thermodynamic tracers to delineate magmatic, meteoric, metamorphic, or sedimentary fluid end-members.
130
Publications
6.1K
Citations
553
Authors
262
Institutions
Publications per year
2017–2026
36
Parents
130
1–5 of 130
553
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Scottish Universities Environmental Research Centre, United Kingdom
3 publications · 182 citations
3
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3
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3
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1–5 of 553
262

Chinese Academy of Sciences
Beijing, China
14 h-index
34 publications
2K citations
Institute of Geochemistry
Guiyang, China
7 h-index
13 publications
1K citations

China University of Geosciences (Beijing)
Beijing, China
6 h-index
17 publications
775 citations
Institute of Geology and Geophysics
Beijing, China
6 h-index
16 publications
697 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
13 publications
495 citations
Russian Academy of Sciences
Moscow, Russia
5 h-index
11 publications
479 citations
China University of Geosciences
Wuhan, China
5 h-index
14 publications
878 citations
Geological Survey of Canada
Ottawa, Canada
5 h-index
8 publications
185 citations
1–8 of 262
16 publications · 793 citations
15
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16 publications · 468 citations
12
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10 publications · 425 citations
10
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10 publications · 712 citations
9
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6 publications · 531 citations
6
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