Main commodities | Fe |
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Ore minerals | pyrrhotite |
Quadrangle map, 1:250,000-scale | MH |
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Quadrangle map, 1:63,360-scale | A-5 |
Latitude | 63.1019 |
Longitude | -146.108 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is at an elevation of 3,500 feet; about one-half mile west of the south end of Landmark Gap Lake. It is at the northwest corner of section 18, T. 21 S., R. 9 E., Fairbanks Meridian. The location is accurate within about 800 feet. |
Geologic descriptionThis prospect is hosted by an Upper Triassic mafic-ultramafic intrusive complex that is comagmatic with the basalt flows of the Nikolai Greenstone (Nokleberg and others, 1991; L. Hulbert, oral communication, 2001). Net-textured to massive pyrrhotite was found in a gabbro sill near the base of the Nikolai Greenstone at this site. There are virtually no base or precious metals associated with the sulfides (L.D. Hulbert, oral communication, 2001). | |
Geologic map unit | (-146.110243984323, 63.1014725179824) |
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Mineral deposit model | Ni-Cu-PGE in differentiated mafic-ultramafic sill. |
Age of mineralization | Late Triassic, the age of the host rock. |
Workings or exploration | This occurrence is on active MAN Resources claims. |
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Indication of production | None |
References | |
Reporters | W.T. Ellis (Alaska Earth Science), C.C. Hawley (Hawley Resource Group), and W.J. Nokleberg (USGS) |
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Last report date | 7/18/2001 |