GMRAP ID | 8 |
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Tract name | Eastern Alaska Range and Wrangell Mountains (003pCu5002) |
Site status | deposit |
Country | United States |
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State or province | Alaska |
Geographic location | -142.8449, 62.204 |
Geologic map unit | -142.8449, 62.204 |
Nearby data |
Deposit type | Porphyry copper |
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Age (Ma) | 105Ma |
Age determination method | K-Ar |
Age range | 114 ±3.4 to 105 ±4.0Ma (Inferred from age of Nabesna pluton.) |
Age reference | Richter, Lanphere, and Matson (1975) |
Minerals | anhydrite, biotite, bornite, chalcopyrite, chlorite, epidote, kaolinite, magnetite, molybdenite, pyrite, sericite |
Associated rocks | quartz feldspar porphyry, trondhjemite, basalt, granodiorite, limestone, mudstone, quartz diorite, siltstone, volcaniclastics |
Tectonic setting | continental margin |
Stratigraphic age | Early Cretaceous |
Development status | Prospect |
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Major commodities | Ag, Au, Cu, Mo |
Tonnage (Mt) | 320Mt |
Cu grade (%) | 0.35% |
Mo grade (%) | 0.02% |
Contained copper | 1,100,000t |
Gold-Moly ratio | -9999 |
Comments | The average grade of the unoxidized mineralization is estimated to be 0.35 percent copper and 0.02 percent molybdenum. Gold values range up to 0.04 ounce per ton and probably average about 0.005 ounce per ton. A central 400- by 2,000-meter altered zone contains abundant biotite, quartz veinlets, minor K-feldspar, chlorite, and sericite; it is cut by late anhydrite veins. An outer 1,000- by 3,000-m altered zone contains chlorite, minor sericite, and anhydrite. First discovered and staked as early as 1902 for its possible gold content; by 1940, 18 mining claims had been patented; extensively explored by open cuts, shafts, short adits, and much diamond drilling; underground workings total only 250 to 300 ft and most were reported be caved by 1944. |
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Study area name | United States |
References | U.S. Geological Survey (2014a); Mendenhall and Schrader (1903); Richter, Lanphere, and Matson (1975); Nokleberg and others (1987); Richter, Singer and Cox (1975); Young and others (1997); Singer and others (2008) |
Site reference | U.S. Geological Survey National Mineral Resource Assessment Team (2002) |