| Deposit ID | 10079594 |
|---|---|
| MRDS ID | W029631 |
| Record type | Site |
| Current site name | Mt.Windarra, Australia |
| Alternate or previous names | North Operations |
| Geographic coordinates: | 122.16587, -28.49621 (WGS84) |
|---|---|
| Relative position | ABOUT 270 KM NNE FROM KALGOORLIE |
Political divisions (FIPS codes)
Western Australia(province)
Australia(country)
Australia(continent)
Land(continent)
| Country | State |
|---|---|
| Australia | Western Australia |
| Commodity | Importance |
|---|---|
| Nickel Critical | Primary |
| Copper | Primary |
| Iron | Tertiary |
| Sulfur | Tertiary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Magnetite | Ore |
| Pentlandite | Ore |
| Pyrite | Ore |
| Pyrrhotite | Ore |
| Result | PYRRHOTITE: PENTLANDITE RATIO VARY FROM 1:1 IN DISSEMINATED ORE TO 20:1 IN LIMITED AREAS IN MASSIVE BRECCIA ORE. THE OVERALL RATIO IS ABOUT 3:1. THE NICKEL-COPPER RATIOS VARY BETWEEN 8:1 AND 14:3 AND INCREASE SOUTH TO NORTH. MINERAL COMPOSITION OF THE TRANSITION AND SUPERGENE ZONE ( % WEIGHT) |
|---|---|
| Result | PENTLANDITE 6-8, PYRRHOTITE 20-25, PYRITE 1.5-2.5, CHALCOPYRITE 0.5-1.0, IRON OXIDES TR.-1.0, SILICATE/CARBONATE, GANGUE 60-70 |
| Host or associated | Associated | ||||||||
|---|---|---|---|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock | ||||||||
| |||||||||
| Host or associated | Associated |
|---|---|
| Rock type | Metamorphic Rock > Gneiss |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite |
| Rock unit name | Granites, Granites Gneisses Ultramafics |
| Rock description | Granites, Granites Gneisses Ultramafics |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock |
| Rock unit name | Ultramafics, Metasediments, Granites, Gneisses |
| Rock description | Ultramafics, Metasediments, Granites, Gneisses |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Chemical Sediment > Iron Formation |
| (1) | 122.16587, -28.49621 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Yilgarn Block Of The Western Australien Shield. Large N-S Anticline. Perhaps A Domal Structure. . Large N-S Anticline. Perhaps A Domal Structure. |
| Type of structure | Local |
| Structure description | Footwall Contact To The Mt.Windarra Banded Iron Formation |
| General form | GOSSAN, LENS |
|---|---|
| Dip | 0 DEG TO 88 DEG, E TO NE |
| Thickness | 18M |
| Length | 1520M |
| Width | 18M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Large |
| Significant | No |
| Discovery year | 1969 |
| Discoverer | Ken Shirley, Poseidon Ltd. Unided Oil Development Corporation Australia Hana Ltd. Home Stake Iron Ore Company Poseidon Ltd. |
| Year of first production | 1974 |
| Year | 1974 | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE | |||||||||||||||||||||
| Description | Ap_Grade: ^1.91 % Ni, 0.19 % Cu | |||||||||||||||||||||
| ||||||||||||||||||||||
| Type | In-situ | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1974 | |||||||||||||||||||||
| Total resources | 696000000mt ore | |||||||||||||||||||||
| ||||||||||||||||||||||
| Type of workings | Underground |
|---|---|
| Overall depth | 790M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W029631 |
E/MJ FEBR. 1974 P.21
AUSTRALIAN MINERAL INDUSTRY, VOL. 28 NO.4 (1976)
E/MJ FEBR. 1975, P. 53, (DISCOVERY AND DEVELOPMENT IN DETAIL.)
G7 TO G10) AUSTRALIAN MINERALS INDUSTRY, REVIEW 1975; D1) KIPPENBERGER 1977;
METALS SOURCEBOOK V. 2, NO. 4
| Subject category | Comment text |
|---|---|
| Deposit | A CONCENTRATOR WAS COMMISSIONED AT THE MT.WINDARRA SIDE IN 1974. CONCENTRATES ARE TRANSPORTED BY ROAD TO MALCOLM NEAR LEONORA, AND ARE THAN RAILED TO KALGOORLIE FOR MIXING WITH WMC CONCENTRATE PRIOR TO REFINING OR SMELTING. |
| Deposit | AVERAGE THICKNESS ABOUT 3 M |
| Deposit | ORE SHOOTS: FISHER, MCMAHON-GELLATY, KEN, HUNT, LUNNON, DURKIN, OTTER-JUAN. BY THE END OF 1975 WMC HAD DISCOVERED AT LEAST 15 OREBODIES IN THE KAMBALDA/ST. IVES AREA. ORE IS GENERALLY MINED BY SLOT STOPPING OR BY CUT-AND-FILL STOPPING. KAMBALDA'S CONCENTRATOR CURRENTLY HAS A CAPACITY OF 1,400,000 TONNES OF ORE PER YEAR. |
| Deposit | MT. WINDARRA ORE IS ESSENTIALLY VERTICAL IN DIP, COMPOSED OF NORTH- TRENDING LENTICULAR SHOOTS DISPOSED ABOUT A DRAG FOLD. MID. 1970 FIVE ORE SHOTTS HAD BEEN OUTLINED WIDTH 3 TO 18 METER. AVERAGE5.5 METER |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1978 | Saam, Henning G. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.