Mine detail: San Miguel, Quetana Cu Mine

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Location

Lat / long: -22.44421, -69.00952

Resource(M)

Primary: Copper
Ore: Chalcopyrite, Enargite
Gangue: Hematite, Jarosite, Kaolinite, Pyrite, Sericite
Discovery year: 1961

Production

Operation type: Unknown
Production size: Yes
Development status: Producer

Geology

Host type:Monzonite,Andesite
Associated type:Mafic Intrusive Rock,Diorite,Granite
Structure:Complexly Folded And Faulted Central Ranges, Cerro De Quetana, West Fissure At Chuquicamata Reportedly Passes A Short Distance East Of Quetana And Is Considered To Be The Major Structure For Cu Mineralization
Tectonic:Andean Cordillera And Batholith
Alteration processes:Local Si-Rich Intrusions Caused Wide-Spread Alteration And Completely Silicified The Adjacent Limestone

References

MRDSW001553
DEP10068483
Reference{Deposit:: RUIZ, F., 1965, GEOLOGIA Y YACIMIENTOS METALIFEROS DE CHILE: INST. INV. GEOL., TABLE 1 (SPANISH)}{Deposit:: MINING JOUR. ANN. REV. 1969, JUNE P. 258}{Deposit:: MINING WORLD, 1959, V. 21, NO. 2, P. 73.}{Deposit:: HOLMES, S. W., 1962, HAS ANOTHER PORPHYRY COPPER BEEN DISCOVERED IN NORTHERN CHILE (?): WORLD MINING, V. 15, NO. 5, P. 35-43.}{Deposit:: RACZYNSKI, ANDRES, 1962, MINA QUETANA, INST. INV. GEOL., UNPUBLISHED INFORMATION (SPANISH).}{Deposit:: 1962 COMPILE INSTITUTO DE INVESTIGACIONES GEOLOGICAS CHIL}{Production:: MINING WORLD, 1959, REF.}{Reserve-Resource:: INVESTMENT REPORTED IN MINING JOUR. ANNUAL REVIEW JUNE 1969 - P. 258}
ReporterDavidson, Claire B.