| Deposit ID | 10106983 |
|---|---|
| MRDS ID | TC03517 |
| Record type | Site |
| Current site name | Buena Esperanza |
| Alternate or previous names | Buena Esperanza Cu Mine |
| Geographic coordinates: | -70.20955, -22.18255 (WGS84) |
|---|---|
| Elevation | 450 |
| Relative position | 10KM SOUTH OF TOCOPILLA AND 170KM NORTH OF ANTOFAGASTA |
Political divisions (FIPS codes)
Chile(country)
South America(continent)
Land(continent)
| Country |
|---|
| Chile |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Materials | Type of material |
|---|---|
| Atacamite | Ore |
| Bornite | Ore |
| Chalcocite | Ore |
| Chalcopyrite | Ore |
| Chrysocolla | Ore |
| Copper | Ore |
| Covellite | Ore |
| Digenite | Ore |
| Malachite | Ore |
| Calcite | Gangue |
| Gypsum | Gangue |
| Hematite | Gangue |
| Plagioclase | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Sericite | Gangue |
| Result | LOWER PART OF FLOWS ARE GENERALLY 7M THICK AND VERY COMPACT CONTAINING 0.1-0.4% COPPER. SULFUR ISOTOPE OF ORE = -0.3/MIL. |
|---|
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||||
| Rock unit name | La Negra Formation;Andean Diorite Complex | ||||||
| Rock description | La Negra Formation;Andean Diorite Complex | ||||||
| |||||||
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||||||
| |||||||
| Host or associated | Host | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||||||
| |||||||
| Host or associated | Host | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||||
| Rock unit name | La Negra Formation;Metamorphosed Sedimentary Sequence | ||||||
| Rock description | La Negra Formation;Metamorphosed Sedimentary Sequence | ||||||
| |||||||
| Host or associated | Host | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||||||
| |||||||
| (1) | -70.20955, -22.18255 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | North-Trending Broad Open Folds. Faults Of Varying Lengths And Displacements And Plutonic Masses. |
| Type of structure | Local |
| Structure description | Faults At N90e, 90 Fractures Trend N40e. Deposit Terminated On North By Post-Mineral, Vertical, East-Striking Fault. |
| General form | TABULAR, ANYGDALOIDAL LAVA FLOWS CONTAINING POCKETS OF BRECCIATED VOLCANIC ROCKS SEVERAL METERS THICK |
|---|---|
| Strike | 0 |
| Dip | 30E |
| Thickness | 270M |
| Length | 200M |
| Width | 330M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Large |
| Significant | No |
| Discovery year | 1954 |
| Year of first production | 1954 |
| District name | Punta Blanca-Cerro Tres Puntas |
|---|
| Type | Owner-Operator |
|---|---|
| Owner | Compania Minera De Tocopilla |
| Year | 1970 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | To 1970 | ||||||||||||||
| Material | CU | ||||||||||||||
| Description | Cp_Grade: ^3% | ||||||||||||||
| |||||||||||||||
| Year | 1986 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1970-1986 | ||||||||||||||
| Material | CU | ||||||||||||||
| Description | Cp_Grade: ^3% | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1983 | ||||||||||||||
| Total resources | 850000000mt ore | ||||||||||||||
| |||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC03517 |
FRUTOS, J. AND PINCHEIRA, M., 1986, FICHAS METALOGENICAS DE YACIMEINTOS MINERALES METALICOS CHILENOS, IN FRUTOS, J., OYARZUN, J., AND PINCHEIRA, M., EDS., GEOLOGIA Y RECURSOS MINERALES CHILENOS: UNIVERSIDAD DE CONCEPCION, CONCEPCION, P. 841-888.
RUIZ, C. AND PEEBLES, F., 1988, YACIMIENTOS METALIFEROS DE CHILE: SANTIAGO, 334 P.
CAMUS, F., 1986, LOS YACIMIENTOS ESTRATOLIGADOS DE CU, PB-ZN, Y AG DE CHILE, IN FRUTOS, J., OYARZUN, J., PINCHEIRA, M., EDS., GEOLOGIA Y RECURSOS MINERALES CHILENOS: UNIVERSIDAD DE CONCEPCION, CONCEPCION, P.548-635.
LOSERT, J., 1973, GENESIS OF COPPER MINERALIZATION AND ASSOCIATED ALTERATIONS IN THE JURASSIC VOLCANIC ROCKS OF THE BUENA ESPERANZA MINING AREA: UNIVERSIDAD DE CHILE, PUBLIC NO. 40, 64 P.
LOSERT, J., 1974, ALTERATION AND ASSOCIATED COPPER MINERALIZATION IN THE JURASSIC VOLCANIC ROCKS OF THE BUENA ESPERANZA MINING AREA, ANTOFAGASTA PROVINCE, NORTHERN CHILE: UNIVERSIDAD DE CHILE, V. 41, P. 51-85.
PALACIOS, C. AND DEFINIS, 1981, PETROLOGIA DEL YACIMIENTO BUENA ESPERANZA, II REGION NORTE DE CHILE: FIRST COLOQUIO SOBRE VOLCANISMO Y METALOGENESIS, UNIVERSIDAD DEL NORTE, P. 82-91.
SASAKI, A., ULRIKSEN, C., SATO, K., AND ISHIHARA, S., 1984, SULFUR ISOTOPE RECONNAISSANCE OF PORPHYRY COPPER AND MANTO-TYPE DEPOSITS IN CHILE AND THE PHILLIPPINES: BULL. GEOLOGICAL SURVEY JAPAN, V. 35, P. 615-622.
DEFINIS, 1980, PETROLOGIA, ALTERACION, Y METALOGENESIS DEL INTRUSIVO BASICO BUENA ESPERANZA, TOCOPILLA, II REGION, CHILE: TESIS DE GRADO, UNIVERSIDAD DEL NORTE, 67 P.
ROGERS, G., 1985, A GEOCHEMICAL TRAVERSE ACROSS THE NORTH CHILEAN ANDES: PH.D. THESIS, THE OPEN UNIVERSITY, LONDON.
MINING MAGAZINE, JANUARY, 1990.
BORIC, R., DIAZ, F., AND MAKSAEV, V., 1984, COMPLEMENTO MAPA METALOGENICO, II REGION: GERENCIA DE DESAROLLO, SANTIAGO, (12 VOLS.).
RUIZ F., CARLOS, 1965, GEOLOGIA Y YACIMIENTOS METALIFEROS DE CHILE: INST. INV. GEOL. CHILE, P. 196 (SPANISH)
KNOWLES, P.H., AND OTHERS, 1964, EXPLORACION DE MINERALES RADIOACTIVOS EN CHILE, PROV. TARAPACA AND ANTOFAGASTA: CHILE INST. INV. BOL. 18, PT. I, P. 33-37 (SPANISH).
1961 COMPILE UNIV. OF CHILE
1964 RECON U.S. ATOMIC ENERGY COMM. & INSTITUTO INVESTIGACIONES GEOLOGICAS, CHILE.
CIMRI
RUIZ AND PEEBLES, 1988; BORIC ET AL., 1984. MINING MAGAZINE, JANUARY, 1990.
BORIC, ET AL., 1984.
| Subject category | Comment text |
|---|---|
| Deposit | MINA VIEJA CONSISTS OF 28 LEVELS CONCENTRATED AT TOP OF FLOWS IN AMYGDULES, BRECCIA LENSES, AND INTERCALATED SANDSTONE LENSES; THICKNESSES VARY FROM 2-25M; DEPOSIT EXTENDS AS FAR AS 200M ALONG STRIKE TO THE WEST BUT IS CUT OFF TO THE EAST BY AN UNMINERALIZED GABRROIC INTRUSION; IN 1969, MINE NUEVA BEGAN PRODUCTION FROM SUBVERTICAL VEINS AND COLUMNS OF BRECCIA AT THE PERIPHERY. |
| Deposit | RECORD W001969 BY CLAIRE B. DAVIDSON HAS BEEN INCORPORATED INTO THIS RECORD. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-SEP-1989 | Williams, William C. | University of Arizona | |
| Updater | 01-APR-1973 | Davidson, Claire B. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.