| Deposit ID | 10065215 |
|---|---|
| MRDS ID | TC40317 |
| Record type | Site |
| Current site name | Artolla Mine |
| Geographic coordinates: | -68.23449, -22.72393 (WGS84) |
|---|---|
| Elevation | 3200 |
| Relative position | 20 KM NORTH OF SAN PEDRO DE ATACAMA. |
Political divisions (FIPS codes)
Chile(country)
South America(continent)
Land(continent)
| Country |
|---|
| Chile |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Materials | Type of material |
|---|---|
| Atacamite | Ore |
| Bornite | Ore |
| Chalcocite | Ore |
| Chalcopyrite | Ore |
| Copper | Ore |
| Covellite | Ore |
| Cuprite | Ore |
| Galena | Ore |
| Malachite | Ore |
| Pyrite | Ore |
| Silver | Ore |
| Tenorite | Ore |
| Albite | Gangue |
| Calcite | Gangue |
| Celestite | Gangue |
| Gypsum | Gangue |
| Hematite | Gangue |
| Quartz | Gangue |
| Result | ORIGINALLY, 10-18% CU MINERALIZATION OCCURED BELOW 100 DEGREES C. SULFUR ISOTOPES: -33.788 TO -29.690 CP, BN, DI FROM VEINLETS IN BRECCIATED SS -27.603 TO -12.634. FLINT (1986) CONTAINS PROBE ANALYSES OF COPPER ORE MINERALS, PB ISOTOPE ANALYSES, SULFUR ISOTOPES. |
|---|
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||
| Rock unit name | Artollo Member Of Pacencia Group | ||
| Rock description | Artollo Member Of Pacencia Group | ||
| |||
| (1) | -68.23449, -22.72393 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Anticline Trending N40e. |
| Name | SAND LENSES |
|---|---|
| General form | LENTICULAR |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discoverer | Worked By Atacamenos And/Or Incas. |
| District name | San Bartolo |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC40317 |
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | MINERALIZATION IS CONCENTRATED IN PALE GRAY, BLEACHED SANDSTONES OF ARTOLLA MEMBER AND IS DISCONTINUOUS, IRREGULAR, AND ERRATIC BUT IS RICHEST NORTH OF THE SAN BARTOLO DOME; 80% OF MINERALIZATION IN OXIDE-CEMENTED SANDSTONES, WHILE THE REMAINDER IS IN SMALL VEINLETS; MINERALIZATION IN UP TO 15 SEPARATE HORIZONS. IN ARTOLLA MINE MINERALIZATION IS MAINLY MATRIX FILLING. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-NOV-1993 | Page, Norman J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.