The Huarón Mining District is one of the richest polymetallic (Zn-Pb-Ag-Cu-(Au)) deposit clusters in Peru. It is located 20 km SSW of Cerro de Pasco, in the Huayllay District, Pasco Province, Pasco Department, between 4500 and 4700 m.a.s.l. The Huarón Mining District belongs to the Miocene polymetallic belt of the Central Andes. Hydrothermal mineralization occurs as predominantly in N-S to NNW-SSW and E-W veins as well as in "mantos" replacing favorable sedimentary rock. Epithermal hydrothermal fluids are thought to be derived from quartz-monzonitic intrusions tentatively dated at 7.4 Ma (K-Ar on adularia). The most important economic minerals are tennantite‐tetrahedrite (containing most of the silver), sphalerite, galena, and chalcopyrite. Silver is also found in pyrargyrite, proustite, p
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| - Distrito minero de Huarón (es)
- Huarón Mining District (en)
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| - The Huarón Mining District is one of the richest polymetallic (Zn-Pb-Ag-Cu-(Au)) deposit clusters in Peru. It is located 20 km SSW of Cerro de Pasco, in the Huayllay District, Pasco Province, Pasco Department, between 4500 and 4700 m.a.s.l. The Huarón Mining District belongs to the Miocene polymetallic belt of the Central Andes. Hydrothermal mineralization occurs as predominantly in N-S to NNW-SSW and E-W veins as well as in "mantos" replacing favorable sedimentary rock. Epithermal hydrothermal fluids are thought to be derived from quartz-monzonitic intrusions tentatively dated at 7.4 Ma (K-Ar on adularia). The most important economic minerals are tennantite‐tetrahedrite (containing most of the silver), sphalerite, galena, and chalcopyrite. Silver is also found in pyrargyrite, proustite, p (en)
- El distrito minero de Huarón incluye algunas de las minas polimetálicas (Zn-Pb-Ag-Cu-(Au)) más ricas del Perú. Está localizado 20 km SSW de Cerro de Pasco, en el Distrito Huayllay, Provincia Pasco, Departamento Pasco, entre 4500 y 4700 m.s.n.m. El distrito es parte del cinturón polimetálico Mioceno de los Andes Centrales. La mineralización hidrotermal epitermal forma predominantemente rellenos en vetas N-S a NNW-SSW y E-W, así "mantos" reemplazando rocas sedimentarias favorables. Los fluidos hidrotermales se derivan probablemente de intrusiones cuarzo-monzoníticias datadas tentativamente en 7.4 Ma (K-Ar en adularia). Los minerales económicos más importantes son tennantita‐tetraedrita (conteniendo la mayoría de la plata), esfalerita, galena y calcopirita. La plata es también se encuentra (es)
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| - The Huarón Mining District is one of the richest polymetallic (Zn-Pb-Ag-Cu-(Au)) deposit clusters in Peru. It is located 20 km SSW of Cerro de Pasco, in the Huayllay District, Pasco Province, Pasco Department, between 4500 and 4700 m.a.s.l. The Huarón Mining District belongs to the Miocene polymetallic belt of the Central Andes. Hydrothermal mineralization occurs as predominantly in N-S to NNW-SSW and E-W veins as well as in "mantos" replacing favorable sedimentary rock. Epithermal hydrothermal fluids are thought to be derived from quartz-monzonitic intrusions tentatively dated at 7.4 Ma (K-Ar on adularia). The most important economic minerals are tennantite‐tetrahedrite (containing most of the silver), sphalerite, galena, and chalcopyrite. Silver is also found in pyrargyrite, proustite, polybasite, and pearceite. In the central copper core of the Huarón deposit, enargite occurs. Main gangue minerals are pyrite, quartz, rhodochrosite, and calcite. (en)
- El distrito minero de Huarón incluye algunas de las minas polimetálicas (Zn-Pb-Ag-Cu-(Au)) más ricas del Perú. Está localizado 20 km SSW de Cerro de Pasco, en el Distrito Huayllay, Provincia Pasco, Departamento Pasco, entre 4500 y 4700 m.s.n.m. El distrito es parte del cinturón polimetálico Mioceno de los Andes Centrales. La mineralización hidrotermal epitermal forma predominantemente rellenos en vetas N-S a NNW-SSW y E-W, así "mantos" reemplazando rocas sedimentarias favorables. Los fluidos hidrotermales se derivan probablemente de intrusiones cuarzo-monzoníticias datadas tentativamente en 7.4 Ma (K-Ar en adularia). Los minerales económicos más importantes son tennantita‐tetraedrita (conteniendo la mayoría de la plata), esfalerita, galena y calcopirita. La plata es también se encuentra en pyrargyrita, proustita, polibasita, y pearceita. En la zona central de Huarón hay enargita . Los principales minerales de ganga son pyrite, cuarzo, rhodochrosite, y calcita. (es)
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