Skarn Alteration
Skarn Alteration is a geological alteration process characterized by the metasomatic replacement of carbonate or silicate rocks through high-temperature fluid-rock interaction, typically associated with intrusive igneous activity, leading to the formation of calcium- or magnesium-rich silicate minerals distinct from other hydrothermal alteration types.
206
Publications
8.2K
Citations
650
Authors
225
Institutions
Publications per year
2017–2026
46
Variants
Skarn Metasomatism
Parents
206
1–5 of 206
650
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h-index
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225

Chinese Academy of Sciences
Beijing, China
13 h-index
47 publications
2K citations

Chinese Academy of Geological Sciences
Beijing, China
13 h-index
43 publications
1.9K citations

China University of Geosciences (Beijing)
Beijing, China
13 h-index
34 publications
1.4K citations
China University of Geosciences
Wuhan, China
12 h-index
36 publications
1.6K citations
University of Chinese Academy of Sciences
Beijing, China
9 h-index
22 publications
888 citations

Washington State University
Pullman, United States
9 h-index
9 publications
890 citations

Central South University
Changsha, China
8 h-index
32 publications
1K citations

Colorado School of Mines
Golden, United States
6 h-index
7 publications
405 citations
1–8 of 225
46 publications · 2.8K citations
28
h-index
37 publications · 1.3K citations
21
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17 publications · 528 citations
15
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7 publications · 227 citations
6
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5 publications · 542 citations
5
h-index
1–5