| Deposit ID | 10068815 |
|---|---|
| MRDS ID | W002073 |
| Record type | Site |
| Current site name | El Aguilar Mine |
| Alternate or previous names | Aguilar, Hamahuaca Mine |
| Geographic coordinates: | -65.7161, -23.19752 (WGS84) |
|---|---|
| Elevation | 4750 |
| Location accuracy | 2000(meters) |
| Relative position | 50 KM TO SSW OF TRES CRUCES, Acc Within 1 Minute |
Political divisions (FIPS codes)
Jujuy(province)
Argentina(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Argentina | Jujuy |
| Commodity | Importance |
|---|---|
| Zinc Critical | Primary |
| Lead | Primary |
| Silver | Primary |
| Copper | Secondary |
| Arsenic Critical | Tertiary |
| Molybdenum | Tertiary |
| Materials | Type of material |
|---|---|
| Alabandite | Ore |
| Antimony | Ore |
| Argentite | Ore |
| Boulangerite | Ore |
| Bournonite | Ore |
| Breithauptite | Ore |
| Cubanite | Ore |
| Gold | Ore |
| Hematite | Ore |
| Magnetite | Ore |
| Marcasite | Ore |
| Molybdenite | Ore |
| Polybasite | Ore |
| Pyrargyrite | Ore |
| Pyrite | Ore |
| Pyrrhotite | Ore |
| Silver | Ore |
| Actinolite | Gangue |
| Calcite | Gangue |
| Chlorite | Gangue |
| Diopside | Gangue |
| Epidote | Gangue |
| Garnet | Gangue |
| Pyroxene | Gangue |
| Quartz | Gangue |
| Rhodonite | Gangue |
| Scapolite | Gangue |
| Tourmaline | Gangue |
| Vesuvianite | Gangue |
| Wollastonite | Gangue |
| Model code | 208 |
|---|---|
| USGS model code | 31a |
| Deposit model name | Sedimentary exhalative Zn-Pb |
| Mark3 model number | 13 |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite | ||||
| Rock unit name | Aguilar Granite | ||||
| Rock description | Aguilar Granite; | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock > Quartzite |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| Rock unit name | Padrioc Formation;;; |
| Rock description | Padrioc Formation;;; |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Chemical Sediment > Chert |
| (1) | -65.7161, -23.19752 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | During Mineralization: Growth Faults And Slumping In A Shallow Marine Basin. Post-Ore: Two Phases Of Gentle, Open Folding (Lord?, Mpal-Lpal?), E-W Compression And Extension (Ljur-Ecret), Intrusion With Local Doming And Fracturing (Ecret), Thrust-Faulting (Ltert) |
| Type of structure | Local |
| Structure description | On East Limb Of A Post-Ore N-S Trending Syncline, Bounded, Deformed, And Disrupted By Post-Ore Folding, Faulting, And Intrusion |
| General form | LENSE |
|---|---|
| Strike | N5E |
| Dip | STEEP TO WEST |
| Thickness | 200M |
| Length | 2000M |
| Width | 1000M |
| Depth to top | 0M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Large |
| Significant | No |
| Discovery year | 1650 |
| Discoverer | Known To Incas And Spanish Colonists |
| Year of first production | 1936 |
| Production years | 1936- |
| District name | Sierra De Aguilar District |
|---|
| Type | Operator |
|---|---|
| Owner | Cia Minera Aguilar Sa |
| Type | Owner |
|---|---|
| Owner | Cia Minera Aguilar S. A. (Subsidiary St. Joe Lead Co.) |
| Year | 1981 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1936-1981 | ||||||||||||||||||||||||||||
| Material | CONS (2) | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Cp_Grade: ^52-56% Zn, 2.5-3% Pb, 170-260 G/T Ag | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Year | 1981 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1936-1981 | ||||||||||||||||||||||||||||
| Material | CONS (1) | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Cp_Grade: ^75-777% Pb, 2.5-3,7% Zn, 1350-1420 G/T Ag | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Type | In-situ | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1936 | ||||||||||||||||||||||||||||
| Total resources | 3585500000mt ore | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Length | 65000M |
| Overall depth | 750M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W002073 |
ANGELELLI, V., FERNANDEZ LIMA, J. C., HERRERA, A., AND ARISTARAIN, L., 1970, DESCRIPCION DEL MAPA METALOGENETICO DE LA REPUBLICA ARGENTINA: DIRRECION NACIONAL DE GEOLOGIA Y MINERIA, P. 117-118 (SPANISH)
SOMMI, L.V., 1956, LA MINERIA ARGENTINA Y LA INDEPENDENCIA ECONOMICA: BUENOS AIRES, EDITORIAL RAIGAL, P. 120-128.
ANGELELLI, V. 1984, YACIMIENTOS METALIFEROS DE LA REPUBLICA ARGENTINA: LA PLATA, COMISION DE INVESTIGACIONES CIENTIFICAS, PROVINCIA DE BUENOS AIRES, V. 2, P. 476-480.
(1,2) ANGELELLI (1984) P. 476. (3) GEMMELL AND OTHERS (1992) P. 2085; WORLD MINING (1985); ROSKILL,(1972, P. 403, 1973, P. 31); MINING ANNUAL REVIEW (1980), P. 395.
| Subject category | Comment text |
|---|---|
| Deposit | STRATABOUND ORE ZONE BOUNDED BY AGUILAR WEST AND CANEDO FAULTS AND AGUILA GRANITE EXTENDS 2 KM ALONG STRIKE, AT LEAST 1 KM DOWN DIP AND IS UP TO 200 M THICK. DEPOSIT HAS BEEN EXPLORED TO 750 M DEPTH AND IS OPEN AT THAT DEPTH. A WELL-DEVELOPED SULFIDE STRATIGRAPHY CONSISTS OF BASAL QUARTZITE WITH FINELY DISSEMINATED SULFIDES. OVERLYING STOCKWORK SULFIDES IN QUARTZITE. SULFIDE FILLING OPEN SPACE IS SEDIMENTARY (QUARTZITE) SLUMP BRECCIA, AND CAPPING MASSIVE STRATIFORM SULFIDES. ALL BEDS ARE CUT BY SEVERAL GENERATIONS OF MINERALIZED FRACTURES. PART OF THE DEPOSIT, INCLUDING ANY OXIDIZED ZONE, MAY HAVE BEEN REMOVED BY GLACIAL EROSION. |
| Deposit | THIS UPDATE (1/93) IS A SUBSTANTIAL REVISION OF THIS RECORD BASED ON RECENT RESEARCH BY GEMMELL AND OTHERS (1992) AND SUREDA AND MARTIN (1990). THE DEPOSIT HAD PREVIOUSLY BEEN INTERPRETED AS A ZN-PB SKARN. |
| Deposit | Discovery Year: 1600'S |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-73 | Davidson, Claire B. | U.S. Geological Survey | |
| Updater | 01-JAN-93 | Long, Keith R. | U.S. Geological Survey | |
| Updater | 01-JUL-93 | Page, Norman J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.