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This document discusses sources of fluid components in iron oxide copper-gold (IOCG) deposits. It notes that IOCG deposits form in diverse geological environments and settings. Genetic models need to consider multiple fluid components that may have different sources for each deposit. Evidence suggests ore fluids had salinities derived from more than one source, which also differed for each deposit. Sources of the principal economic metals in IOCG deposits, like copper and gold, remain only circumstantially

Author

M Andrés Castaño C

Language

EN