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Characteristics of high-temperature, carbonate-hosted massive sulphide ores in the United States, Mexico, and Peru form a distinctive genetic class. These ores occur within carbonate rocks and were formed from hydrothermal fluids at elevated temperatures. They share similarities in mineralization style and alteration with volcanic-hosted massive sulfide deposits but also have features of discordance and local complexity. Exploration of these deposits is difficult due to complex geochemical, geometrical, and

Author

junior.geologia

Language

EN