Potassic Alteration
Potassic Alteration is a type of hydrothermal alteration process in which potassium-rich minerals such as K-feldspar, biotite, or sericite are introduced into a rock through fluid-rock interaction, distinguished by the addition of potassium and typically associated with high-temperature, reduced conditions in magmatic-hydrothermal systems.
164
Publications
8.6K
Citations
469
Authors
179
Institutions
Publications per year
2017–2026
29
Parents
164
1–5 of 164
469
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National and Kapodistrian University of Athens, Greece
6 publications · 157 citations
6
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6
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National and Kapodistrian University of Athens, Greece
4 publications · 100 citations
4
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4
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1–5 of 469
179

Chinese Academy of Sciences
Beijing, China
8 h-index
26 publications
1.3K citations

University of Tasmania
Hobart, Australia
7 h-index
20 publications
1.4K citations
Institute of Geology and Geophysics
Beijing, China
6 h-index
18 publications
865 citations

China University of Geosciences (Beijing)
Beijing, China
6 h-index
12 publications
781 citations
Iowa State University
Ames, United States
6 h-index
6 publications
139 citations
China University of Geosciences
Wuhan, China
5 h-index
12 publications
213 citations
Geological Survey of Canada
Ottawa, Canada
5 h-index
9 publications
743 citations

McGill University
Montreal, Canada
5 h-index
9 publications
456 citations
1–8 of 179
63 publications · 4.5K citations
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8 publications · 170 citations
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7 publications · 346 citations
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7 publications · 189 citations
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6 publications · 194 citations
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