Main commodities | Au |
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Other commodities | Hg |
Ore minerals | arsenopyrite |
Gangue minerals | quartz |
Quadrangle map, 1:250,000-scale | MH |
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Quadrangle map, 1:63,360-scale | A-6 |
Latitude | 63.1895 |
Longitude | -146.9248 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is at an elevation of about 4,800 feet at the head of an unnamed south-flowing tributary to Coal Creek, in the S1/2SW1/4 section 11, T. 20 S., R. 4 E., Fairbanks Meridian. The location corresponds to mineral occurrence 27 of Clautice and others (1988, 1989). The location is accurate within one-tenth of a mile. |
Geologic descriptionA small, probably Cretaceous granodiorite plug and felsite dikes intrude greenstone and argillite in the area of this occurrence (Kaufman, 1964). The deposit consists of an iron-stained quartz stockwork in argillite (Clautice and others, 1989, plate 2). The stockwork is strongly anomalous in arsenic (1,925 parts per million [ppm]) and mercury (64 ppm) and contains 170 parts per billion (ppb) gold (Clautice and others, 1988, sample 33882). Stream-sediment sample 33610S collected about one-half mile downstream was anomalous in arsenic (495 ppm) and somewhat anomalous in tungsten (25 ppm). | |
Geologic map unit | (-146.927064586779, 63.1890576475622) |
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Mineral deposit model | Low-sulfide Au-quartz veins (Cox and Singer, 1986, model 36a). |
Mineral deposit model number | 36a |
Age of mineralization | Probably Cretaceous, related to intrusion of granodiorite and felsite dikes. |
Workings or exploration | There are no workings at the site. |
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Indication of production | None |
Additional commentsAn arsenic anomaly at the mouth of the tributary stream suggests further prospecting is warranted in the area. |
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 | 6/14/2001 |