| Deposit ID | 10086816 |
|---|---|
| MRDS ID | ANC0200 |
| Record type | Site |
| Current site name | Mi Ensueno, Mina |
| Geographic coordinates: | -77.16642, -9.54797 (WGS84) |
|---|---|
| Elevation | 4500 |
| Location accuracy | 1000(meters) |
| Relative position | A 32 KM DE CHAVIN., Est . Tomada De La Hoja De Recauay 20-I, Esc. 1:100000 |
Political divisions (FIPS codes)
Ancash(province)
Peru(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Peru | Ancash |
| Peru | Ancash |
| Commodity | Importance |
|---|---|
| Silver | Primary |
| Lead | Primary |
| Zinc Critical | Primary |
| Materials | Type of material |
|---|---|
| Calcite | Gangue |
| Result | 34.90 OZ/TC AG, 15.52% PB, 19.28% ZN. |
|---|
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock > Slate |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock > Quartzite |
| (1) | -77.16642, -9.54797 |
|---|
| General form | ISOMETRICO (RELLENO DE FRACTURAS) |
|---|---|
| Strike | N18E |
| Dip | 80SE |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Ownership category | Private |
|---|
| Type | Owner-Operator |
|---|---|
| Owner | Francisco Palacios |
| Year | 1955 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | AG PB ZN | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Ap_Grade: ^14.12% Pb, 31.66 Oz/Tc Ag, 17.99% Zn. | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | ANC0200 |
ZUNIGA, SERGIO; INFORME DE LA MINA MI ENSUENO, B.M.P. NOVIMEBRE 1955, COD. B4343
BANCO MINERO
| Subject category | Comment text |
|---|---|
| Deposit | SE TRATA DE UN YACIMIENTO FILONIANO, FORMADO POR RELLENO DE FRACTURAS ORIGINADAS ANTES DE PRODUCIRSE LAS INYECCIONES MINERALIZANTES. LAS FRACTURAS SE HAN EMPLAZADO EN CUARCITAS Y PIZARRAS MOSTRANDOSE CLARAS Y BIEN DEFINIDAS. ESTA FRACTURACION ANTERIOR A LA MINERALIZACION PARECE SER EL RESULTADO DE LA INTRUSION DE ROCA IGNEA, PUES A PESAR DE NO HABER LOCALIZADO ROCAS DE ESTE TIPO, LA PROXIMIDAD A LA CORDILLERA BLANCA HACEN SUPONER LA INFLUENCIA DEL INTRUSIVO EN LA MINERALIZACION DE LA REGION. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-94 | Delgado Valladares, Javier E. | Instituto Geologico Minero Y Metalurgico, Peru | |
| Updater | 01-APR-94 | Gonzales, Rosa | Instituto Geologico Minero Y Metalurgico, Peru |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.