| Deposit ID | 10068823 |
|---|---|
| MRDS ID | W002081 |
| Record type | Site |
| Current site name | Infiernillo Cu Prospect |
| Geographic coordinates: | -68.83278, -34.5808 (WGS84) |
|---|---|
| Elevation | 1700 |
| Relative position | 50 KM W OF SAN RAFAEL, ACCESS BY HIGHWAY 144 |
Political divisions (FIPS codes)
Argentina(country)
South America(continent)
Land(continent)
| Country |
|---|
| Argentina |
| Commodity | Importance |
|---|---|
| Copper | Tertiary |
| Molybdenum | Tertiary |
| Lead | Tertiary |
| Zinc Critical | Tertiary |
| Arsenic Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Galena | Ore |
| Pyrite | Ore |
| Sphalerite | Ore |
| Calcite | Gangue |
| Hematite | Gangue |
| Quartz | Gangue |
| Result | IN DDH 7 CU VALUES OBTAINED WERE 1.05%, 230-235 FT. |
|---|---|
| Result | 0.9%, 270-295 FT. |
| Result | 0.68%, 650-655 FT. VALUES OF CU & MO IN HYDROTHERMALLY ALTERED DACITE PORPHYRY WERE CU, 0.1% AND MO, 0.01% |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock |
| Rock unit name | Quartz Intrusive (Plug) In Dacitic Porphyry;Dacitic Porphyry;Tuffs |
| Rock description | Quartz Intrusive (Plug) In Dacitic Porphyry;Dacitic Porphyry;Tuffs |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite |
| Rock unit name | Sedimentary Rocks;Metasedimentary Rocks |
| Rock description | Sedimentary Rocks;Metasedimentary Rocks |
| (1) | -68.83278, -34.5808 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | N-Trending Folded And Faulted Ranges East Of Principal Cordillera. Pal Rocks Intruded By Intermediate To Felsic Plutons. Faults Of 5000-M Displacement On Eastern Frontal Cordillera |
| Type of structure | Local |
| Structure description | Dacitic Porphyry Intrudes Older Rocks & Is Cut By Small Nnw & Nne-Striking Basalt Dikes Faults And Fractures Of Quartz-Calcite Veinlets Are In Area. In Center Of Dacitic Porphyry Is Intrusive Plug Of Massive Barren Quartz, 200 M N-S, 60 M Across, Which Dominates Relief |
| General form | DACITE STOCK IS ROUGHLY OVAL |
|---|---|
| Length | 4500M |
| Width | 3500M |
| Development status | Prospect |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discoverer | Present Work By United Nations And Gov'T Of Argentina |
| Type | Owner |
|---|---|
| Owner | Government Of Argentina |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W002081 |
UNITED NATIONS DEVELOPMENT PROGRAMME, 1970, INVESTIGATION OF PORPHYRY COPPER TYPE MINERALIZATION IN THE PROVINCES OF MENDOZA, NEUQUEN, AND SAN JUAN, ARGENTINA: NEW YORK, UNITED NATIONS, P. 238-244.
UNITED NATIONS DEVELOPMENT PROGRAMME, 1970, INVESTIGATION OF PORPHYRY COPPER-TYPE MINERALIZATION IN THE PROVINCES OF MENDOZA, NEUQUEN, AND SAN JUAN, ARGENTINA: NEW YORK, UNITED NATIONS, P. 238-244.
1966 DIREXPL UNITED NATIONS, GOV'T OF ARGENTIN
| Subject category | Comment text |
|---|---|
| Deposit | 40 VEINS IN 2 SYSTEMS, ONE ORIENTED E-W, THE OTHER NW-SE WITH AN INCLINATION TO THE N OF 70 TO 80 DEGREES TO VERTICAL. |
| Deposit | MOST IMPORTANT VEINS ARE: ALCAPARROSA, VETILLA, VALLEJO, SANTA RITA, ROSARIO, BELEN, TAJO, SAN LORENZO, FLORIDA, AND TRINIDAD. ; INFO.SRC : 1 PUB LIT |
| Deposit | FAVORABLE CHARACTERISTICS FOR "RESERVING" THE AREA ARE EVIDENCE OF STRONG CU AND MO ANOMALIES WHICH FORM A RING AROUND THE QUARTZ PLUG & EVIDENCE OF MINERALIZATION IN BOULDERS AND IN QUARTZ VEINS. INTENSE PENEPLANATION IN AREA MAY HAVE REMOVED IMPORTANT CU MINERALIZED ZONES ABOVE THE ROOTS OF THE INTRUSIVE, BUT IT IS POSSIBLE SECONDARY ENRICHED DEPOSITS MAY HAVE FORMED BELOW THE ERODED ZONES AND THEREFORE COULD BE QUITE CLOSE TO THE SURFACE |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1973 | Davidson, Claire B. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.