Geothermal activity and epithermal gold mineralization in Japan
Eiji Izawa, Masahiro Aoki
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Hydrothermal enrichment of lithium in intracaldera illite-bearing claystones. [PDF]
Benson TR, Coble MA, Dilles JH.
europepmc +1 more source
Hydrological controls on base metal precipitation and zoning at the porphyry-epithermal transition constrained by numerical modeling. [PDF]
Stoltnow M, Weis P, Korges M.
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MINERALOGICAL CHARACTERS OF KARANG PANINGAL EPITHERMAL VEIN DEPOSITS, WEST JAVA
Karang Paningal gold-ore deposits belong to the epithermal deposits. As hydrothermal deposits, the alter- ation that occurs in this area comprises argillitization, sericitization and silicification.
WAHYUDI, TATANG
core
Fluid-rock interactions leading to the formation of the epithermal Ag-Pb-Zn veins: A perspective of thermodynamic modeling. [PDF]
Zhai D.
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Clay minerals in epithermal deposits.
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A Clay Mineral Accompanied by Epithermal Iron Sulphide Deposits
Kinoshita, Kameki, Tanaka, Shin-ya
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Lihir Alkalic Epithermal Gold Deposit, Papua New Guinea
The Lihir gold deposit, Papua New Guinea, is the world’s largest alkalic low-sulfidation epithermal gold deposit in terms of contained gold (50 Moz). The deposit formed over the past million years and records a progression from porphyry- to epithermal ...
Ageneau, M (15811607) +7 more
core
Colloidal transport and flocculation are the cause of the hyperenrichment of gold in nature. [PDF]
McLeish DF +4 more
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Raman Spectroscopy Coupled with Reflectance Spectroscopy as a Tool for the Characterization of Key Hydrothermal Alteration Minerals in Epithermal Au-Ag Systems: Utility and Implications for Mineral Exploration. [PDF]
Arbiol C, Layne GD.
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