The Unnamed (north of Leduc Lake) is a molybdenum and copper mine located in Alaska.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Mine Info
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Unnamed (north of Leduc Lake) MRDS details
Site Name
Primary: Unnamed (north of Leduc Lake)
Commodity
Primary: Molybdenum
Primary: Copper
Secondary: Zinc
Secondary: Tungsten
Secondary: Silver
Secondary: Lead
Location
State: Alaska
District: Ketchikan
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: Conspicuous iron-staining.
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Chalcopyrite
Ore: Molybdenite
Ore: Pyrrhotite
Gangue: Quartz
Comments
Comment (Reference): Primary Reference = Berg and others, 1977
Comment (Workings): Workings / Exploration = Eleven chip samples of quartz veins and metamorphic hostrocks contained up to 110 ppm Cu, 15 ppm Pb, 60 ppm Zn, 1.5 ppm Ag, 100 ppm Mo, and, in one sample, a trace of W (Berg and others, 1977, p. 125).
Comment (Deposit): Model Name = Disseminated base-metal sulfides in metamorphic roof pendant
Comment (Deposit): Other Comments = Occurrence is in Misty Fiords National Monument Wilderness.
Comment (Geology): Geologic Description = The country rocks in the area of this occurrence are pelitic paragneiss, subordinate quartzofeldspathic paragneiss, and minor amphibolite and tactite (Berg and others, 1977, p. 123-124; Berg and others, 1988). These rocks, accompanied by small intrusions of pegmatite and diorite, form a large roof pendant in Tertiary or Cretaceous foliated granodiorite and quartz diorite of the Coast Range batholith. The metamorphic rocks probably represent marine argillaceous, clastic, and minor mafic volcanic strata that underwent high-grade regional metamorphism in Cretaceous or Tertiary time. The premetamorphic age of the strata is uncertain, but they probably are mainly Paleozoic and may be as old as Precambrian (Berg and others, 1988, p. 26; Gehrels and others, 1990; Crawford and others, in press).? the occurrence is a band of iron-stained paragneiss 450-900 feet wide and about 3 miles long (Berg and others, 1977, p. 123-125). It consists of small quartz veins and stringers that both parallel and crosscut the schistosity of the enclosing metamorphic rocks, which locally are intruded by small pegmatite dikes and sills. Berg and others (1977) reported anomalous amounts of molybdenum in rock (table 3, no. 16) and stream-sediment (figs. 9, 12) geochemical samples collected in this area. Eleven follow-up chip samples collected by the U.S. Bureau of Mines contained up to 110 ppm Cu, 15 ppm Pb, 60 ppm Zn, 1.5 ppm Ag, 100 ppm Mo, and, in one sample, a trace of W (Berg and others, 1977, area M-1, p. 123-125). In addition, several concordant lenses of chocolate-brown-weathering amphibolite up to about 2 feet wide and 15 feet long contain a small amount of pyrrhotite and a trace of chalcopyrite.
References
Reference (Deposit): Elliott, R.L., Berg, H.C., and Karl, Susan, 1978, map and table describing metalliferous and selected nonmetalliferous mineral deposits, Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-file Report, 78-73-B,17 p., scale 1:250,000.
Reference (Deposit): Berg, H.C., Elliott, R.L., and Koch, R.D., 1988, Geologic map of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Mineral Investigations Series Map MF-1807,27 p., scale 1:250,000.
Reference (Deposit): Gehrels, G.E., McClelland, W.C., Samson, S.D., Patchett, P.J., and Jackson, J.L., 1990, Ancient continental margin assemblage in the northern Coast Mountains, southeast Alaska and northwest Canada: Geology, v. 18, p. 208-211.
Reference (Deposit): Crawford, M.L., Crawford, W.A., and Gehrels, G.E., 2000, Terrane assembly and structural relationships in the eastern Prince Rupert quadrangle, British Columbia, in H.H. Stowell and W.C.McClelland, eds., Tectonics of the Coast Mountains, southeastern Alaska and British Columbia: Boulder, Colorado, Geological Society of America Special Paper 343, p. 1-21.?
Reference (Deposit): Berg, H.C., Elliott, R.L., Smith, J.G., Pittman, T.L., and Kimball, A. L., 1977, Mineral resources of the Granite Fiords wilderness study area, Alaska, with a section on aeromagnetic data by Andrew Griscom: U.S. Geological Survey Bulletin 1403, 151 p.
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