| Deposit ID | 10068920 |
|---|---|
| MRDS ID | W002195 |
| Record type | Site |
| Current site name | Rescate Copper Belt 22 |
| Geographic coordinates: | -71.4996, -16.56437 (WGS84) |
|---|---|
| Elevation | 2750 |
| Relative position | 35 KM. FROM SOCABAYA BY ROAD, 8 KILOMETERS SE OF CERRO VERDE, 20 KM DUE SOUTH OF AREQUIPA |
Political divisions (FIPS codes)
Arequipa(province)
Peru(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Peru | Arequipa |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Gold | Primary |
| Silver | Primary |
| Zinc Critical | Secondary |
| Lead | Secondary |
| Materials | Type of material |
|---|---|
| Bornite | Ore |
| Chalcopyrite | Ore |
| Galena | Ore |
| Gold | Ore |
| Silver | Ore |
| Sphalerite | Ore |
| Ankerite | Gangue |
| Pyrite | Gangue |
| Siderite | Gangue |
| Tourmaline | Gangue |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite | ||
| |||
| (1) | -71.4996, -16.56437 |
|---|
| General form | LENTICULAR |
|---|---|
| Strike | N |
| Dip | 75E |
| Length | 90M |
| Width | 1M |
| Depth to bottom | 300M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1927 |
| Year of first production | 1927 |
| Type of workings | Underground |
|---|---|
| Length | 3000M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W002195 |
SIMONS, FRANK, 1960, UNPUBLISHED REPORT, P. 912
PERU-MAPA METALOGENETICO, 1969, AND, GUIA PARA EL MAPA METALOGENETICO DEL PERU, SOCIEDAD NACIONAL DE MINERIA Y PETROLEO, LIMA, PERU, NOV. 1969
1960 COMPILE FRANK SIMONS, UNPUB. REP
F. SIMONS, 1960, UNPUB. REP.
METALLOGENIC MAPS OF PERU. 1969, 1972
| Subject category | Comment text |
|---|---|
| Deposit | THE LENTICULAR ORE BODY LIES ALONG A NORTH TRENDING ZONE THAT DIPS ABOUT 75 DEG EAST AND IS CUT OFF AT THE NORTH END BY AN EAST-TRENDING VERTICAL PRE-MINERAL FAULT. THE FOOTWALL IS USUALLY MARKED BY AN INDISTINCT FRACTURE OVERLAIN BY SEVERAL METERS OF GOOD ORE, WHEREAS THE HANGING WALL IS AN ASSAY WALL AT THE LIMIT OF 6-12 M OF LOWER GRADE ORE. ORE GRADE DECREASES GRADUALLY TOWARD THE SOUTH END OF THE ORE BODY. PYRITE AND SPHALERITE BECOME MORE ABUNDANT AT DEPTH, AND CHALCOPYRITE DECREASED |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-1973 | Shaffer, Glenn L. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.