Epithermal Ore Systems
Epithermal Ore System is a hydrothermal ore deposit system formed at shallow crustal depths (typically <1.5 km) and low to moderate temperatures (50–300°C), characterized by precipitation of precious and base metals from magmatically influenced meteoric fluids driven by volcanic-hydrothermal activity.
93
Publications
7K
Citations
300
Authors
136
Institutions
Publications per year
2017–2026
14
Variants
Epithermal Ore Deposits
Parents
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300
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136

The University of Western Australia
Perth, Australia
6 h-index
12 publications
1.1K citations

China University of Geosciences (Beijing)
Beijing, China
6 h-index
21 publications
561 citations
Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry
Moscow, Russia
5 h-index
14 publications
439 citations

Chinese Academy of Sciences
Beijing, China
5 h-index
17 publications
854 citations
Geological Survey of Japan
Tsukuba, Japan
5 h-index
6 publications
1.5K citations
ETH Zurich
Zurich, Switzerland
4 h-index
20 publications
2.4K citations
Geological Survey of Western Australia
East Perth, Australia
4 h-index
4 publications
617 citations

McGill University
Montreal, Canada
3 h-index
8 publications
363 citations
1–8 of 136
19 publications · 2.7K citations
17
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11 publications · 452 citations
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6 publications · 264 citations
6
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5 publications · 181 citations
5
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4 publications · 86 citations
4
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1–5