| Deposit ID | 10086993 |
|---|---|
| MRDS ID | CUZ0074 |
| Record type | Site |
| Current site name | San Juan De Dios, Mina |
| Geographic coordinates: | -72.22184, -13.49503 (WGS84) |
|---|---|
| Elevation | 3700 |
| Location accuracy | 1000(meters) |
| Relative position | A 11.5 KM AL SW DE LA LOCALIDAD DE ANTA., Est . Tomados Del Plano Departamento-Cuzco. |
Political divisions (FIPS codes)
Cusco(province)
Peru(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Peru | Cusco |
| Peru | Cusco |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Malachite | Ore |
| Result | CU=1.66% ,AG=0.74 0Z/TC LEY PROMEDIO DE 4 MUESTRAS TOMADAS EN LA BRECHA Y VETILLAS DE COBRE GRIS. |
|---|
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite |
| (1) | -72.22184, -13.49503 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Estructural En Brecha De Falla. |
| General form | IRREGULAR |
|---|---|
| Length | 60M |
| Width | 3M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Sr. Constantino Ladron De Guevara Pineda. |
| Year | 1969 | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE CU-AG | |||||||||||||||||||||
| Accuracy | Estimate | |||||||||||||||||||||
| Description | Ap_Grade: ^Leyes Variables Cu=10-13% Ag=2.3 - 3.5 Oz/Tc. | |||||||||||||||||||||
| ||||||||||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | CUZ0074 |
HORACIO FERNANDEZ NIQUE, INFORME MINA SAN JUAN DE DIOS.BMP.1,969 COD.B3093
INFORME BMP SOBRE LA MENSIONADA MINA 1,969.
| Subject category | Comment text |
|---|---|
| Deposit | LAS POSIBILIDADES DEL YACIMIENTO SON DESFAVORABLES POR LO SIGUIENTE:NO EXISTEN ESTRUCTURAS DEFINIDAS,LOS CARBONATOS DE COBRE ESTAN IRREGULARMENTE DESTRIBUIDOS,EL MINERAL NO PUEDE SER CIRCADO Y TAMPOCO PUEDE HACERSE UN BUEN ESCOGIDO A MANO Y SU OPERACION ES SUB-MARGINAL. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-94 | Condori Taipe, Tulio | Instituto Geologico Minero Y Metalurgico, Peru |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.