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Shotgun; Mose Prospect, Bristol Bay Mining District, Dillingham Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Shotgun; Mose Prospect | Prospect |
| Bristol Bay Mining District | Mining District |
| Dillingham Census Area | Census Area |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
60° 24' 34'' North , 158° 7' 29'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Location: The Shotgun prospect is in the southern part of the Shotgun Hills, a rugged. glaciated upland at the head of the King Salmon River. The prospect is near the center of the NW1/4 of section 27, T. 4 N., R. 51 W. of the Seward Meridian. It is on the crest and eastern slope of a northwest-trending ridge at an elevation of about 2,500 feet.
Geology: This prospect was discovered in the 1980s during a regional exploration program by Cominco Alaska in a joint venture with ENSTAR. They named this prospect Mose and did surface mapping and sampling, and drilled six shallow diamond drill holes. In the 1990s, ENSTAR's interest was sold to NovaGold Resources Inc., the prospect was renamed Shotgun, and a renewed exploration effort took place. This exploration included extensive diamond drilling in 1998 that included 19 drill holes totaling 10,170 feet (NovaGold Resources Inc., 2000). TNR Gold Corporation optioned Shotgun (Mose) from NovaGold Resources, Inc. in 2003. A running history of TNR Gold's work to April 2007 can be seen in several news releases and project information at their web site (TNR Gold Corp., 2007). Initial exploration under this agreement was in September 2003 and included surface geologic mapping, and an airborne magnetic survey. TNR Gold Corporation's exploration work during the summer of 2004 included surface geologic mapping, and sampling at Shotgun (Mose) and other prospects including Shot (TA031), King (TA030), and Beats Me (TA029). In the summer of 2005, the TNR Gold Corporation exploration program included drilling 6 holes to further refine and expand the resource at Shotgun (Mose) and evaluate other prospects in the area. The Shotgun prospect is an intensely quartz-veined, felsic porphyry stock that sharply crosscuts biotite hornfels developed in mid-Cretaceous clastic sedimentary rocks of the Kuskokwim Group (Rombach, 2000). As exposed along the ridge crest and downslope to the east, the stock is an irregularly shaped composite intrusion that is about 1,000 feet long in a northwest direction and over 500 feet long in a northeast direction. The hornfels near the stock and across the ridge crest to the southwest commonly is breccia healed by a toumaline-rich matrix and locally cut by veinlets that contain arsenopyrite, pyrite, and some chalcopyrite. In the stock, some zones near the contact are extensively silicified; quartz replacement is massive and complete in these zones. Elsewhere, the stock is cut by quartz veins that in places form an intense, anastomosing stockwork. Albite-sericite-quartz +/- carbonate replacement of host intrusive rocks accompanies the quartz veining. The deposit is deeply oxidized and iron-staining is widespread. Ore minerals identified at Shotgun include arsenopyrite, primary native gold and bismuth, Bi-Te sulfides, chalcopyrite, lollingite, pyrrhotite, pyrite, scheelite, sphalerite, and supergene covellite, chalcocite, native copper, and marcasite (Rombach, 2000). Vapor-rich and saline-rich fluid inclusions coexist in the quartz veins. In order of abundance, the vapor-rich inclusions contain water, carbon dioxide, and methane; these inclusions homogenize to vapor at about 360 degrees C. The saline-rich inclusions have salinities of 40 to greater than 60 weight percent NaCl equivalent and homogenize to liquid at 280 to more than 600 degrees C (Rombach, 2000). Surface rock samples define a large geochemical anomaly with several areas where gold values exceed 1 part per million. Examples of drill hole intercepts include 233 feet grading 0.077 ounce of gold per ton, 399 feet grading 0.050 ounce of gold per ton, and 43 feet grading 0.155 ounce of gold per ton (NovaGold Resources Inc., 2000; all drill hole intercepts are listed online at http://www.nrigold.com/shotgun.htm; Dec 2000). Preliminary metallurgical tests indicate that gold recoveries of more than 93 percent can be achieved using conventional cyanidation. Airborne and ground magnetometer surveys have been used in conjunction with extended mapping and sampling to evaluate the potential for additional mineralization in surrounding areas. As of March 28, 2007, NovaGold Resources, Inc. (2007) reports that the Shotgun prospect has 32.8 million tonnes of resources with a grade of 0.93 gram of gold per ton. A large granitic pluton makes up the core of the Shotgun Hills. The contact between this pluton and the hornfels that surrounds the Shotgun prospect coincides with a northwest-trending linear swale and drainage less than 0.5 mile north of the prospect. The shallow-seated intrusive environment south of this contact (extensive hornfels locally cut by fine-grained porphyry) compared to that to the north, suggests that this contact is a large fault, dropped down to the south. K/Ar and Ar/Ar dating of intrusive rocks and mineralization in the Shotgun prospect area indicate that magmatism and mineralization is latest Cretaceous in age, about 68 to 70 Ma (Rombach, 2000; Travis Hudson, unpublished data, 2000).
Workings: This prospect was discovered in the 1980s in a regional exploration program by Cominco Alaska in joint venture with ENSTAR. They named this prospect Mose and completed surface mapping, sampling, and the drilling of six shallow diamond drill holes. In the 1990s, ENSTAR's interest was sold to NovaGold Resources Inc., the prospect was renamed Shotgun, and renewed exploration took place. This exploration included extensive new diamond drilling in 1998 that included 19 drill holes totaling 10,170 feet. Airborne and ground magnetometer surveys have been used in conjunction with extended mapping and sampling to evaluate the potential for additional deposits in surrounding areas. TNR Gold Corporation optioned Shotgun (Mose) from NovaGold Resources, Inc. in 2003. A running history of TNR Gold's work to April 2007 can be seen in several news releases and project information at their web site (TNR Gold Corp., 2007). Initial exploration under this agreement was in September 2003 and included surface geologic mapping and an airborne magnetic survey. TNR Gold Corporation's exploration work during the summer of 2004 included surface geologic mapping and sampling at Shotgun (Mose) and other prospects including Shot (TA031), King (TA030), and Beats Me (TA029). In the summer of 2005, the TNR Gold Corporation exploration program included drilling 6 holes to further refine and expand the resource at Shotgun (Mose) and evaluate other prospects in the area.
Age: Latest Cretaceous, 68 to 70 Ma, based on K/Ar and Ar/Ar dating of intrusive rocks and mineralization.
Alteration: Silicification and albite-sericite-quartz +/- carbonate replacement of host intrusive rocks.
Reserves: As of March 28, 2007, NovaGold Resources, Inc. (2007) reports the that the Shotgun prospect has 32.8 million tonnes of resources with a grade of 0.93 gram of gold per ton.
Commodities (Major) - Au; (Minor) - As, Bi, Ce, Cu, T, W, Zn
Development Status: None
Deposit Model: Gold-bearing quartz-stockwork veining in felsic porphyry.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
16 valid minerals.
Detailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) |
| ⓘ Arsenopyrite Formula: FeAsS |
| ⓘ Chalcocite Formula: Cu2S |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Covellite Formula: CuS |
| ⓘ Löllingite Formula: FeAs2 |
| ⓘ Marcasite Formula: FeS2 |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Bismuth Formula: Bi |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Gold Formula: Au |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Pyrrhotite Formula: Fe1-xS |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Scheelite Formula: Ca(WO4) |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Gold | 1.AA.05 | Au |
| ⓘ | Native Bismuth | 1.CA.05 | Bi |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Löllingite | 2.EB.15a | FeAs2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
| Group 9 - Silicates | |||
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
List of minerals for each chemical element
Other Databases
| Link to USGS - Alaska: | TA007 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Farewell buried DomainDomain
- Koyukuk ArcsVolcanic Arc
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