| Deposit ID | 10079576 |
|---|---|
| MRDS ID | W029608 |
| Record type | Site |
| Current site name | Trojan |
| Geographic coordinates: | 31.33465, -17.29706 (WGS84) |
|---|---|
| Elevation | 1530 |
| Relative position | 6 MILES SOUTH OF BINDURA, ABOUT 40 MILES NE OF SALISBURY |
Political divisions (FIPS codes)
Zimbabwe(country)
Africa(continent)
Land(continent)
| Country |
|---|
| Zimbabwe |
| Materials | Type of material |
|---|---|
| Ilmenite | Ore |
| Magnetite | Ore |
| Millerite | Ore |
| Pentlandite | Ore |
| Pyrrhotite | Ore |
| Model code | 11 |
|---|---|
| USGS model code | 6a |
| Deposit model name | Komatiitic Ni-Cu |
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock > Peridotite > Dunite | ||||||
| Rock unit name | Ultramafics | ||||||
| Rock description | Ultramafics | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock > Peridotite > Dunite |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Serpentinite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Komatiite (Ultramafite) |
| Rock unit name | Shamvaian Formation;Bulawayan Formation |
| Rock description | Shamvaian Formation;Bulawayan Formation |
| (1) | 31.33465, -17.29706 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Archaean Greenstone Belt, Precambrian Mafic And Ultramafic Rocks In A Cratonic Environment |
| Type of structure | Local |
| Structure description | Traverse Faults Trend Obliquely Across The Ultrabsic Rocks, Quartz Diorite Stock Intrusive Into Precambrian Bulawan Greenstones, Of Bulawan System. The Rocks Are Isoclinaly Folded.Faults. |
| General form | TABULAR |
|---|---|
| Dip | 83 DEG.N |
| Plunge direction | NE |
| Length | 274M |
| Width | 73.15M |
| Depth to bottom | 360M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1957 |
| Discoverer | Hilton A.J. |
| Year of first production | 1968 |
| District name | Harare (Salisbury) District |
|---|
| Type | Operator |
|---|---|
| Owner | Trojan Nickel Mine Ltd (1965 Anglo American Option To 85 %) |
| Type | Owner |
|---|---|
| Owner | Rhonickel |
| Year | 1969 | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | Until 1969 | |||||||||||||||||||||
| Material | ORE | |||||||||||||||||||||
| Description | Cp_Grade: ^0.583% Ni, 0.211% Cu | |||||||||||||||||||||
| ||||||||||||||||||||||
| Year | 1971 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE | ||||||||||||||
| Accuracy | Estimate | ||||||||||||||
| Description | Ap_Grade: ^0.92% Ni | ||||||||||||||
| |||||||||||||||
| Year | 1976 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE | ||||||||||||||
| Accuracy | Estimate | ||||||||||||||
| Description | Ap_Grade: ^0.68% Ni (Milled Ore) | ||||||||||||||
| |||||||||||||||
| Year | 1979 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1968-1979 | ||||||||||||||
| Material | ORE | ||||||||||||||
| Description | Cp_Grade: ^0.7% Ni | ||||||||||||||
| |||||||||||||||
| Year | 1981 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^0.60% Ni | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1981 | ||||||||||||||
| Total resources | 10400000000mt ore | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1982 | ||||||||||||||
| Total resources | 12650000000mt ore | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1972 | ||||||||||||||
| Total resources | 86000000mt ore | ||||||||||||||
| |||||||||||||||
| Type of workings | Underground |
|---|---|
| Length | 762M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W029608 |
PETERS H.D., NICKEL,1975
ROEX D.H.LE, NICKEL DEPOSIT ON THE TROJAN CLAIMS, BINDURA DISTRICT, S. RHODESIA
SCALLAN R.J., TROJAN NICKEL, VEIL IS LIFTED ON BIG BINDURA OPERATIONS.
DEYOUNG AND OTHERS, 1985, INTERNATIONAL STRATEGIC MINERALS INVENTORY SUMMARY REPORT-- NICKEL: U.S. GEOLOGICAL SURVEY CIRCULAR 930-D, 62 P.
DEYOUNG AND OTHERS, 1985
| Subject category | Comment text |
|---|---|
| Deposit | MINE AND CONCENTRATOR; THE SUCCESSION UNDERLAYING THE CLAIMS THAT COMPRISE THE PROPERTY BELONG TO THE BULAWAYAN AND SHAMVARIAN SYSTEMS, VOLCANICS AND SEDIMENTARY ROCKS BOUNDED BY GRANITE AND GNEISS. INTRUDED IN THESE FORMATIONS ARE A NUMBER OF SILL-LIKE BODIES OF PERIDOTITE NOW ALTERED TO SERPENTINITE. NICKEL CONCENTRATIONS, IN SULFIDE MINERALS, OCCUR IN SERPENTINITE AT LOW LOCALITIES, CARDIFF HILL AND TROJAN HILL. CARDIFF HILL CONTAINS THE PRINCIPAL DEPOSITS, AND HERE MOST OF THE SULFIDE MINERALS ARE DISSEMINATED IN SHEARED SERPENTINITE BUT APPEAR TO HAVE BEEN REMOBILISED ON THE FOOTWALL CONTACT WERE VCKEL AND COPPER CATHODES AND COBALT SLUDGE THERE ARE NO PUBLISHED FIGURES AVAILABLE FOR THE INDIVIDUAL MINES OUTPUT. THE CONCENTRATOR IS DESIGNED TO TREAT 50 000 SHORT TONS OF ORE A MONTH.THE NI WILL BE RECOVERED BY CONVENTIONAL FROTH FLOTATION INTO A CONCENTRATE CONTAINING 15 % NI. |
| Deposit | SHAFT TO 770 FEET DEPTH. THERE ARE THREE OREBODIES. THE HANGING WALL OREBODY, THE MAIN OREBODY, AND THE FOOTWALL OREBODY. THE FIRST TWO ARE MASSIVE DEPOSITS AND CONTAIN THE BULK OF THE ORE POTENTIAL. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1977 | Saam, Henning G. | U.S. Geological Survey | |
| Updater | 01-FEB-1988 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.