| Deposit ID | 10025070 |
|---|---|
| MRDS ID | JUN0080 |
| Record type | Site |
| Current site name | Julia # 1, Mina |
| Geographic coordinates: | -76.20805, -11.70621 (WGS84) |
|---|---|
| Elevation | 4950 |
| Relative position | YAULI, Est Ubicacion De La Mina. |
Political divisions (FIPS codes)
Junin(province)
Peru(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Peru | Junin |
| Peru | Junin |
| Commodity | Importance |
|---|---|
| Silver | Primary |
| Lead | Primary |
| Copper | Primary |
| Zinc Critical | Primary |
| Materials | Type of material |
|---|---|
| Calcite | Gangue |
| Result | AG: 9.8 OZ/TC, PB: 0.05 %, CU: 0.85 %, ZN: 0.18 %. |
|---|
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| (1) | -76.20805, -11.70621 |
|---|
| Strike | N-90-W |
|---|---|
| Dip | 85-N |
| Thickness | 0.1M |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Year of first production | 1970 |
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Raymundo Marin Vega |
| Type | In-situ | |||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1974 | |||||||||||||||||||||||||||||||||||
| Total resources | 900000000mt ore | |||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | JUN0080 |
FLORES T. RAFAEL INF. TEC MINAS DEL AREA POMATAREA BMP 1974-INGEMMET B6408
| Subject category | Comment text |
|---|---|
| Deposit | EL YACIMIENTO ESTA EMPLAZADO DENTRO DE UNA ANDESITA PORFIRITICA CON FUERTE ALTERACION HIDROTERMAL (CAOLLINIZACION). CONSTA DE UNA FRACTURA DEL TIPO DE RELLENO DE FISURA DE ORIGEN HIDROTERMAL, QUE TIENE UNA POTENCIA PROMEDIO DE 30 CM. EL AFLORAMIENTO TIENE UNA EXTENSION VISIBLE APROXIMADA DE 300 MTS DENTRO DE UNA TOPOGRAFIA EN PARTE INACCESIBLE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-94 | Alva Ruiz, Jose L. | Instituto Geologico Minero Y Metalurgico, Peru | |
| Updater | 01-MAY-94 | Gonzales Chavez, Rosa | Instituto Geologico Minero Y Metalurgico, Peru |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.