Low-T Hydrothermal Deposit
Chemical Process (Liquid-phase Growth) - Open system under ground
Synonym
Epithermal deposit, Low-T Hydrothermal Vein Deposit, Low-T Hydrothermal Ore Deposit
Index Minerals
Stibnite, Gold, Realgar, Marcasite
Required Geological Setting
Associated metasomatic zones
Kaolinite zone, Low-T silicified zone, Interstratified mineral zone
Occurrence
Vein-type deposit formed by 100-250 degree hydrothermal fluid originated from Acidic (Rhyolite) to Neutral (Dacite, Andesite) magmatic activities by volcanoes such as caldera complexes in volcanic island arc. Origin of hydrothermal fluid is magmatic water from magma and/or meteoric water. Meteoric water is circulated by heat of magma. Typical elements concentrated are Au, Sb, and/or As. Host of deposits are volcanic products or basements of volcanoes. The deposit may shift to Moderate-T hydrothermal deposit in the deeper level, and to Hydrothermal Au-Ag deposit in the shallower level.

Distribution of Low-T Hydrothermal Deposit described in this site. Yellow lines are volcanic fronts.
Mineral Assemblages (Ore)
Stibnite, Gold, Realgar, Pyrite, Marcasite, Tetrahedrite
Mineral Assemblages (Gangue)
Quartz, Baryte
Localities
- Nishinomaki Mine (Andesite, Realgar)
- Akadani Mine (Rhyolite, Stibnite)
- Furue (Rhyolite, Realgar)