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The document summarizes the geological setting and characteristics of iron oxide-copper-gold (IOCG) deposits in the Coastal Cordillera of northern Chile and southern Peru. The IOCG deposits formed during the Jurassic through Early Cretaceous in association with a volcanic arc characterized by tholeiitic to calc-alkaline plutons. Major fault systems developed during this time period due to subduction rollback and extension. The IOCG deposits are closely related spatially and genetically to gabbro-diorite to
- Author
- Patricio Osorio
- Language
- EN