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Unnamed Occurrence (ARDF - PS007; west of the Middle Fork Chandalar River), Chandalar Mining District, North Slope Borough, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - PS007; west of the Middle Fork Chandalar River)- not defined -
Chandalar Mining DistrictMining District
North Slope BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
68° 2' 24'' North , 147° 49' 11'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201513
Long-form identifier:
mindat:1:2:201513:5
GUID (UUID V4):
0


See also locations PS006 and PS008. Site is in an area thought to have potential for carbonate-hosted lead-zinc deposits (Menzie and others, 1985). The pH of the stream that cuts the mineralization is less than 4.5.
Location: Site is at an elevation of about 3,750 ft. in a small drainage approximately 2 miles west of the Middle Fork Chandalar River and about 7 miles south of the confluence of Beaucoup Creek and Middle Fork Chandalar River (south-center sec. 19, T. 16 S., R. 19 E., of the Umiat Meridian). It is described as Area B on fig. 1 in Detra (1977). Location accurate within 1/4-mile radius.
Geology: One of two mineralized areas with small outcrops within which lead-zinc-silver-(copper) mineralization is found (Detra, 1977). The mineralization is described as occurring in quartz veins in a chert breccia cap on limestone. Samples from the veins are reported to contain galena, sphalerite and chalcopyrite as well as iron sulfides. Exposures of mineralization are less than 3 meters in length and not much wider than the streams (approximately 1 to 2 meters) in which they are exposed. Two samples taken from the mineralized area returned analyses as high as 25% Zn, [more than] 2% Pb and 150 ppm Ag (Detra, 1977). The chert breccia cap which hosts the mineralization occurs locally at the top of the Skajit Limestone at an unconformity that has been interpreted as a paleokarst surface. The chert cap is overlain by yellow-weathering phyllitic siltstones, shales and sandstones, which in turn are overlain by black shales of the Hunt Fork Shale. The surrounding area is mapped as Devonian shale, sandstone and conglomerate with scattered bodies of mafic rocks of uncertain age (Detra, 1977).
Workings: 57 claims in two claim blocks located by Noranda and RAA in 1977. Semi-quantitative spectrographic data (Detra, 1977) from rock samples from the area include: sample number 232RA - Ag (150 ppm), Ba (200 ppm), Cu (700 ppm), greater than 20,000 ppm Pb and Zn. Zn by wet chemical analysis - 250,000 ppm; sample number 232RB - Ag (30 ppm), Ba (300 ppm), Cu (150 ppm), Pb (15,000 ppm), greater than 20,000 ppm Zn. Zn by wet chemical analysis - 75,000 ppm (Detra, 1977, table 1).

Commodities (Major) - Pb, Zn; (Minor) - Ag, Cu(?)
Development Status: None
Deposit Model: Mississippi Valley Zn-Pb (?) (Cox and Singer, 1986; model 32a).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite ?2.CB.10aCuFeS2
Galena2.CD.10PbS
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S SphaleriteZnS
S Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
FeIron
Fe ChalcopyriteCuFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Zn SphaleriteZnS
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:PS007

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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