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This document summarizes a study of the Darrehzar porphyry copper deposit in Iran. Key findings include: 1) Hydrothermal alteration and mineralization at Darrehzar were centered on a Tertiary quartz-monzonite stock and were broadly synchronous with its emplacement. 2) Early alteration produced a potassic assemblage from high-temperature, high-salinity fluids. Later alteration included phyllic and argillic assemblages from lower-temperature fluids. 3) Fluid inclusion studies helped constrain the hydrotherma

Author

Saman Ghaderi

Language

EN