Metals, Minerals, and Society
Chapter 13: Cerro Verde-Santa Rosa Copper-Molybdenum Deposits, Peru: Magmatic, Hydrothermal, and Supergene Characteristics of Two Adjacent Porphyry Systems
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Published:January 01, 2018
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CiteCitation
Ralph J. Stegen, Mark D. Barton, Jerome A. Waegli, 2018. "Cerro Verde-Santa Rosa Copper-Molybdenum Deposits, Peru: Magmatic, Hydrothermal, and Supergene Characteristics of Two Adjacent Porphyry Systems", Metals, Minerals, and Society, Antonio M. Arribas R., Jeffrey L. Mauk
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Abstract
At the Cerro Verde district in southern Peru, granodiorite porphyry stocks formed two adjacent porphyry copper-molybdenum deposits that collectively form one of the largest copper districts in the world, with current resources of ~17 million metric tonnes (Mt) of copper. The district is located within the Coastal batholith of western Peru. The Coastal batholith in the Cerro Verde area consists of the Cretaceous Tiabaya and the Paleocene Yarabamba granodioritic plutons. Granodiorite porphyry stocks associated with the porphyry coppermolybdenum deposits were emplaced into the Yarabamba plutons.
The granodiorite porphyry stocks are composite, steep-walled cylinders. Breccia bodies of diverse textures are...
- Cenozoic
- copper ores
- geochronology
- granodiorites
- igneous rocks
- magmatism
- metal ores
- mineral deposits, genesis
- mineralization
- molybdenum ores
- Paleocene
- Paleogene
- Peru
- plutonic rocks
- porphyry
- porphyry copper
- porphyry molybdenum
- South America
- supergene processes
- Tertiary
- U/Pb
- volcanic rocks
- Cerro Verde
- Santa Rosa Peru
- Yarabamba Pluton