| Deposit ID | 60001613 |
|---|---|
| MRDS ID | W002268 |
| Record type | District |
| Current site name | Tarica District |
| Geographic coordinates: | -77.74146, -8.58131 (WGS84) |
|---|---|
| Relative position | NO. 71 ON METALLOGENIC MAPS OF PERU, 1969 |
Political divisions (FIPS codes)
Ancash(province)
Peru(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Peru | Ancash |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Copper | Primary |
| Silver | Primary |
| Tungsten Critical | Primary |
| Molybdenum | Secondary |
| Lead | Secondary |
| Zinc Critical | Secondary |
| (1) | -77.74146, -8.58131 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | THE OLDEST ROCKS OF THE DISTRICT ARE 200 M. OR SO OF BLACK SHALE WITH INTERBEDDED QUARTZITE, OF LATE JURASSIC AGE (PAMPAS FORMATION, SO CALLED). THEY ARE OVERLAIN BY MORE THAN 100 M OF WHITE QUARTZITE AND BLACK CARBONACEOUS SHALE, WITH COAL BEDS 50-150 CM THICK, OF EARLY CRETACEOUS AGE. THE SEDIMENTARY ROCKS ARE INTRICATELY FOLDED AND AT CAHUACONA AND NORTH AND EAST OF CHOQUEBAMBA WERE INTRUDED BY GRANODIORITE AND LATER BY ANDESITE. AT GRANODIORITE CONTACTS, SHALE MAY CONTAIN CHIASTOLITE PRISMS. THE ENTIRE DISTRICT LIES A FEW KM EAST OF THE CORDILLERA BLANCA GRANODIORITE APOPHYSIS OF THE COASTAL BATHOLITH. THE ORE DEPOSITS SEEM TO BE ZONED ROUGHLY AROUND THE ANDESITE INTRUSIVE OF CAHUACONA, WITH COPPER NEAR THE ANDESITE AND LEAD FARTHER OUT. ORE DEPOSITS ARE BANDED FISSURE VEINS WHICH TEND TO RAMIFY NEAR THE SURFACE AND CONTAIN LITTLE OR NO GANGUE. |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Year of first production | 1882 |
| District name | TARICA DISTRICT |
|---|
| Type | Operator |
|---|---|
| Owner | EMPRESA MINERA SAN JUAN, LTD. |
SIMONS, FRANK, 1960 UNPUBLISHED REPORT, P. 993
PERU-MAPA METALOGENETICO, 1969, AND, GUIA PARA EL MAPA METALOGENETICO DEL PERU, SOCIEDAD NACIONAL DE MINERIA Y PETROLEO, LIMA, PERU, NOV. 1969
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.