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CC Barite Occurrence, Tok Mining District, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types
CC Barite OccurrenceOccurrence
Tok Mining DistrictMining District
Southeast Fairbanks Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 12' 49'' North , 144° 3' 32'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Mentasta Lake112 (2011)35.6km
Mindat Locality ID:
196842
Long-form identifier:
mindat:1:2:196842:5
GUID (UUID V4):
3a753987-4d4b-4661-9dfa-721bf1b2f9b4


Unpublished data cited is available for viewing by contacting Grayd Resources Inc. in Vancouver, B. C., Canada (www.grayd.com), or Northern Associates Inc. in Fairbanks, Alaska.
Location: The CC Barite occurrence is located at an elevation of about 5,600 feet, 0.2 mile north-northwest of peak 6835 and 0.8 mile west-northwest of peak 6740 in the NW1/4 section 34, T. 17 N., R. 7 E., Copper River Meridian. The location is accurate.
Geology: The CC Barite occurrence is in an exposure of the Drum unit; bedded barite is enclosed in quartz-sericite schist that contains sparse disseminated galena and chalcopyrite. This is the only occurrence of bedded barite that has been identified in the Delta mineral belt; it may represent an exhalative precipitate that accumulated peripheral to or capping a sulfide system. It was found during field checking of airborne electromagnetic anomalies that trace a graphitic schist unit below this barite occurrence (S.S. Dashevsky, written communication, 2003). The Drum unit that hosts the CC Barite occurrence consists of white to pale gray-green, rusty weathering, quartz-sericite(-chlorite-pyrite) schist with minor gray to black carbonaceous phyllite and rare interbeds of chloritic phyllite. The schist commonly contains 1 to 5 percent quartz eyes but may contain more. The protoliths of the schist are about two-thirds of volcanic origin and one-third of sedimentary origin. The schist has a phyllitic parting in many places.
Workings: There has only been surface sampling and mapping at this occurrence (S.S. Dashevsky, written communication, 2003).
Age: The enclosing Drum unit has been dated at the Devonian-Mississippian boundary on the basis of one SHRIMP U-Pb zircon age of 359 +/- 6 Ma determined at the DD South prospect (MH325) (Dashevsky and others, 2003).

Commodities (Major) - Ba; (Minor) - Cu, Pb
Development Status: None
Deposit Model: Kuroko massive sulfide (Cox and Singer, 1986; model

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


6 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Baryte7.AD.35BaSO4
Group 9 - Silicates
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
β“˜'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
OOxygen
Oβ“˜ BaryteBaSO4
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
AlAluminium
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ QuartzSiO2
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
Sβ“˜ BaryteBaSO4
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
BaBarium
Baβ“˜ BaryteBaSO4
PbLead
Pbβ“˜ GalenaPbS

Other Databases

Link to USGS - Alaska:MH348

Other Regions, Features and Areas containing this locality


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References

 
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