Epithermal Deposits
Epithermal Deposits is a type of hydrothermal ore deposit characterized by formation at shallow crustal depths (typically 0.5–1.5 km) and low to moderate temperatures (50–300°C), primarily through the precipitation of metals from aqueous fluids driven by volcanic activity, distinguishing it from deeper or higher-temperature hydrothermal systems.
449
Publications
23.9K
Citations
1.3K
Authors
415
Institutions
Publications per year
2017–2026
104
Variants
Epithermal Ore Deposits
Parents
449
1–5 of 449
1.3K
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415

University of Tasmania
Hobart, Australia
18 h-index
52 publications
3.8K citations

Chinese Academy of Sciences
Beijing, China
16 h-index
82 publications
3.2K citations
United States Geological Survey
Reston, United States
15 h-index
30 publications
1.1K citations

Chinese Academy of Geological Sciences
Beijing, China
13 h-index
30 publications
3K citations

China University of Geosciences (Beijing)
Beijing, China
13 h-index
42 publications
1.4K citations

University of Auckland
Auckland, New Zealand
12 h-index
24 publications
1.2K citations
Geological Survey of Japan
Tsukuba, Japan
12 h-index
17 publications
2.7K citations
Nanjing University
Nanjing, China
11 h-index
67 publications
2K citations
1–8 of 415
119 publications · 9K citations
47
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48 publications · 1.9K citations
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26 publications · 825 citations
18
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21 publications · 1.4K citations
16
h-index
14 publications · 502 citations
13
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1–5