Unnamed Prospect (ARDF - MH188; northwest of Fourteenmile Lake), Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
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Latitude & Longitude (WGS84):
63° 5' 39'' North , 145° 49' 47'' West
Latitude & Longitude (decimal):
Köppen climate type:
Location: This occurrence is at an elevation of 4,650 feet, about 1.5 miles northwest of Fourteenmile Lake. It is in the NW1/4SE1/4 section 16, T. 21 S., R. 10 E., Fairbanks Meridian.
Geology: This occurrence consists of float of gabbro, gabbronorite, pyroxenite, olivine melagabbro, and dunite (W.T. Ellis, oral communication, 2001). The rocks are variably serpentinized, and some contain as much as 8 percent sulfide, chiefly in pyrrhotite and chalcopyrite. A sample of sulfide-bearing gabbro contained 0.18 percent nickel, 0.05 percent copper, 46 parts per billion (ppb) palladium, and 15 ppb platinum (W.T. Ellis, oral communication, 2001). Another sample of coarse-grained pyroxenite with 8 percent pyrrhotite and minor chalcopyrite contained 0.12 percent nickel, 0.07 percent copper, 22 ppb palladium, and 35 ppb platinum. The bedrock source of the float is the Tangle ultramafic-mafic intrusive complex of Late Triassic age, which may be a lopolithic feeder of the Nikolai basalt flows of the Wrangellia Terrane (W.T. Ellis, oral communication, 2001). The Tangle complex is a north-dipping layered intrusion of dunite, peridotite, and gabbro that varies from less than 2,000 feet thick to more than 4,000 feet thick and extends for more than 12 miles in length (W.T. Ellis, oral communication, 2001). The complex intrudes Tangle Formation of Permian age (Nokleberg and others, 1991). It may connect with the Fish Lake complex at depth below the Amphitheater synform. Magmatic mineralization is synchronous with emplacement of Tangle complex, which is part of a 120-mile-long belt of mafic-ultramafic and associated rocks in the east-central Alaska Range.
Workings: A sample of sulfide-bearing gabbro contained 0.18 percent nickel, 0.05 percent copper, 46 parts per billion (ppb) palladium, and 15 ppb platinum (W.T. Ellis, oral communication, 2001). Another sample of coarse-grained pyroxenite with 8 percent pyrrhotite and minor chalcopyrite contained 0.12 percent nickel, 0.07 percent copper, 22 ppb palladium, and 35 ppb platinum. The prospect is on active claims of MAN Resources.
Age: Late Triassic.
Alteration: The peridotite is locally serpentinized.
Commodities (Major) - Cu, Ni, Pd, Pt
Development Status: None
Deposit Model: Ni-Cu-PGE in differentiated mafic-ultramafic sill.
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
2 valid minerals.
Detailed Mineral List:
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Pyrrhotite Formula: Fe1-xS |
| ⓘ 'Serpentine Subgroup' Formula: D3[Si2O5](OH)4 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| Unclassified | |||
| ⓘ | 'Serpentine Subgroup' | - | D3[Si2O5](OH)4 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| O | Oxygen | |
| O | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| Si | Silicon | |
| Si | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| Fe | Iron | |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
Other Databases
| Link to USGS - Alaska: | MH188 |
|---|
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