| Deposit ID | 10068483 |
|---|---|
| MRDS ID | W001553 |
| Record type | Site |
| Current site name | San Miguel, Quetana Cu Mine |
| Geographic coordinates: | -69.00952, -22.44421 (WGS84) |
|---|---|
| Elevation | 2800 |
| Relative position | ABOUT 7 KM W. OF CALAMA AND ABOUT 16 KM SW. OF CHIQUICAMATA |
Political divisions (FIPS codes)
Chile(country)
South America(continent)
Land(continent)
| Country |
|---|
| Chile |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Enargite | Ore |
| Hematite | Gangue |
| Jarosite | Gangue |
| Kaolinite | Gangue |
| Pyrite | Gangue |
| Sericite | Gangue |
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock | ||
| |||
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Monzonite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| (1) | -69.00952, -22.44421 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Complexly Folded And Faulted Central Ranges, Cerro De Quetana |
| Type of structure | Local |
| Structure description | West Fissure At Chuquicamata Reportedly Passes A Short Distance East Of Quetana And Is Considered To Be The Major Structure For Cu Mineralization |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Medium |
| Significant | No |
| Discovery year | 1961 |
| Type | Operator |
|---|---|
| Owner | Latin American Mines Ltd. |
| Type | Owner |
|---|---|
| Owner | Sociedad Minera De Quetana |
| Year | 1959 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE | ||||||||||||||
| Accuracy | Estimate | ||||||||||||||
| Description | Ap_Grade: ^Est Greater Than 1 % Cu | ||||||||||||||
| |||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Overall depth | 200M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W001553 |
RUIZ, F., 1965, GEOLOGIA Y YACIMIENTOS METALIFEROS DE CHILE: INST. INV. GEOL., TABLE 1 (SPANISH)
MINING JOUR. ANN. REV. 1969, JUNE P. 258
MINING WORLD, 1959, V. 21, NO. 2, P. 73.
HOLMES, S. W., 1962, HAS ANOTHER PORPHYRY COPPER BEEN DISCOVERED IN NORTHERN CHILE (?): WORLD MINING, V. 15, NO. 5, P. 35-43.
RACZYNSKI, ANDRES, 1962, MINA QUETANA, INST. INV. GEOL., UNPUBLISHED INFORMATION (SPANISH).
1962 COMPILE INSTITUTO DE INVESTIGACIONES GEOLOGICAS CHIL
MINING WORLD, 1959, REF.
INVESTMENT REPORTED IN MINING JOUR. ANNUAL REVIEW JUNE 1969 - P. 258
| Subject category | Comment text |
|---|---|
| Deposit | 3 SIGNIFICANT CU MINERALIZED ZONES ARE QUETANA CENTRAL, NORTH PROSPECT, SOUTH PROSPECT |
| Deposit | CROSS SECTION OF CENTRAL OREBODY CONSISTS OF FOLLOWING ZONES DESCENDING FROM SURFACE TO DEPTH: LEACHED BRECCIA; 800 FT. - THICK LEACHED ZONE OF ALTERED AND LEACHED BRECCIA CONTAINING TRACES OF OXIDE CU; UNKNOWN THICKNESS OF MIXED ZONE OF CU OXIDES AND SULFIDES; UNKNOWN THICKNESS OF ASSUMED SUPERGENE ZONE OF SECONDARY CU SULFIDES |
| Deposit | Discovery Year: ACQUIRED FOR EXPLORATION 1961 |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1973 | Davidson, Claire B. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.