Epithermal vein-type silver deposits comprising adularia-sericite type mineralisations.
The district is located about 7 km NW of the Talcuna Cu Mining District.
References
- Oyarzun, R., Ortega, L., Sierra, J., Lunar, R., and Oyarzun, J. (1998): Cu, Mn, and Ag mineralization in the Quebrada Marquesa Quadrangle, Chile: the Talcuna and Arqueros districts. Mineralium Deposita 33, 547-559.
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