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Автор(ы):John F.H.Thompson, Richard M.T., Vanessa G.Gale, William A.Wright
Издание:Economic geology, 2004 г., 22 стр.
Язык(и)Английский
Characteristics and formation of the Jerónimo carbonate-replacement gold deposit, Potrerillos District, Chile

The Jerónimo sedimentary rock-hosted disseminated Au deposit is located within the Potrerillos district of the Atacama region of northern Chile, east of the Potrerillos porphyry Cu-Mo and El Hueso high-sulfidation Au deposits. Prior to development, the Jerónimo deposit contained a resource of approximately 16.5 million metric tons (Mt) at 6.0 g/t Au. Production began in the oxidized, nonrefractory portion of the deposit in 1997 and terminated in 2002. During that time, approximately 1.5 Mt at 6.8 g/t Au was mined by underground room-and-pillar methods, from which a total of approximately 220,000 oz of Au was recovered by heap-leach cyanidation.

ТематикаПолезные ископаемые
МеткиCarlin type gold, Gold, Jerónimo carbonate-replacement gold deposit, Potrerillos District, Золото
Ленты новостей
2526.85