Essay sample library > Contonga Mine

Contonga Mine

2023-12-17 06:19:01

The Contonga mine is a subsurface multimetal mine with a mining history of over 27 years. This mine is located in the Andes mountains in the center of Peru, 470 km northeast of Lima in Peru. In the Contonga mine area, the vertical zonal mineralization replaced by skarn is controlled by the direction of the bed. Faults occur mainly in strongly folded limestone, surrounded by clearly defined Contonga raw materials.

The multimetal area in the center of Peru forms a strip with a length of 120 kilometers and a length of 800 kilometers. This is equivalent to the western Corsillera and the Andean Plateau. 7 - 14 inches. Polymetal and skarn deposits associated with the Cenozoic magmatism activity are major metal producers (70%, 87%, 96% Zn, Pb, Ag respectively), but mainly in the past 20 years, Zn The importance of geological sediments has increased. Supplier; Currently they account for 4% of Zn, Pb and Ag production, respectively, at 30% and 13%, and two major deposit metals have been identified

Diversity of ages and types of multimetal deposits is particularly attractive for comprehensive studies of trace elements and trace elements such as Ag, Bi, Cd, In, Ge, Ga, Sn, etc. in multimetal ores It is targeting. Distribution area size etc.

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The Contonga mine is a subsurface multimetal mine with a mining history of over 27 years. This mine is located in the Andes mountains in the center of Peru, 470 km northeast of Lima in Peru. In the Contonga mine area, the vertical zonal mineralization replaced by skarn is controlled by the direction of the bed. These faults occur predominantly in strongly folded limestone that surrounds clearly defined Contonga ingredients. The multimetal area in the center of Peru forms a strip with a length of 120 kilometers and a length of 800 kilometers. This is equivalent to the western Corsillera and the Andean Plateau. 7 - 14 inches. Polymetal and skarn deposits associated with the Cenozoic magmatism activity are major metal producers (70%, 87%, 96% Zn, Pb, Ag respectively), but mainly in the past 20 years, Zn The importance of geological sediments has increased. Suppliers; now they occupy 30, 13, each producing 4% Zn, Pb and Ag.