National mineral assessment tract AK-SC16 (Kuroko massive sulfide)

Tract AK-SC16
Geographic region South Central, AK
Tract area 17,220sq km
Deposit type Kuroko massive sulfide
Deposit age Late Paleozoic

Estimates

Confidence Number of
deposits
90% 0
50% 0
10% 1
5% 1
1% 1

Estimators: Nokleberg, Goldfarb, Cox, Campbell, Koch, Yeend

Rationale

Explained by Warren J. Nokleberg, Dennis P. Cox, Richard J. Goldfarb, and David L. Campbell.
On the choice of deposit models
Parts of the eastern Alaska Range and Wrangell Mountains are permissive for Late Paleozoic kuroko massive sulfide deposits (Singer, 1986; Singer and Mosier, 1986) because of favorable bedrock geologic units, known occurrences, anomalous concentrations of Cu, Pb, Zn, As, Au, and Ag in stream sediment samples, and local sulfide minerals in heavy mineral concentrates.
On the delineation of permissive tracts
The geologic unit that defines this tract is the upper Paleozoic marine felsic and intermediate volcanic rocks and interlayered sedimentary rocks forming the upper part of the Skolai igneous arc in the Wrangellia terrane. In addition, stream-sediment geochemical samples yield abundant heavy mineral concentrates containing chalcopyrite, sphalerite, galena, and pyrite. Part of the Wrangellia terrane is tectonically dismembered and local fault-bounded segments may contain undiscovered deposits.
The distribution of the geologic units defining the tract is adapted from Nokleberg and others (1994). The distribution of this belt of mineral deposits is adapted from MacKevett and others (1978) and Nokleberg and others (1987, 1993). Mineral resource assessments of 250,000-scale quadrangles within the tract were done by Richter and others (1975), MacKevett (1976), Singer and MacKevett (1977), Singer and others (1980), Cox and others (1989), and Nokleberg and others (1990).
Important examples of this type of deposit
There are no known deposits of this type in the tract. Kuroko massive sulfide mines exist in rocks of the same age in the Wrangellia terrane on Vancouver Island in southern British Columbia.
On the numerical estimates made
Potential host rocks in the tract are locally covered by extensive ice fields and glaciers, and by Cenozoic basinal deposits. Because kuroko massive sulfide deposits occur elsewhere in probably correlative rocks, the mineral resource team estimated the minimum number of undiscovered deposits that are consistent with the grade and tonnage model of Singer and Mosier (1986) to be:
Percentile 50 10 5 5 1
Estimated number of deposits 0 0 1 1 1
References
Cox, D.P., Light, T.D., Csejtey, Béla, and Campbell, D.L., 1989, Mineral resource assessment map of the Healy quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-2058-A, scale 1:250,000.
MacKevett, E.M., 1976, Mineral deposits and occurrences in the McCarthy quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-773B, scale 1:250,000, 2 sheets.
MacKevett, E.M., Jr., Singer, D.A., and Holloway, C.D., 1978, Maps and tables describing metalliferous mineral resource potential of southern Alaska: U.S. Geological Survey Open-File Report 78-1E, 2 sheets, scale 1:1,000,000, 45 p.
Nokleberg, W.J., Bundtzen, T.K., Berg, H.C., Brew, D.A., Grybeck, Donald, Robinson, M.S., Smith, T.E., and Yeend, Warren, 1987. Significant metalliferous lode deposits and placer districts of Alaska: U.S. Geological Survey Bulletin 1786, 104 p.
Nokleberg, W.J., Bundtzen, T.K., Grybeck, Donald, Koch, R.D., Eremin, R.A., Rozenblum, I.S., Sidorov, A.A., Byalobzhesky, S.G., Sosunov, G.M., Shpikerman, V.I., and Gorodinsky, M.E., 1993, Metallogenesis of mainland Alaska and the Russian Northeast: Mineral deposit maps, models, and tables, metallogenic belt maps and interpretation, and references cited: U.S. Geological Survey Open-File Report 93-339, 222 pages, 1 map, scale 1:4,000,000; 5 maps, scale 1:10,000,000.
Nokleberg, W.J., Lange, I.M., Singer, D.A., Curtin, G.C., Tripp, R.B., Campbell, D.L., and Yeend, Warren, 1990, Mineral resource assessment maps of the Mount Hayes quadrangle, eastern Alaska Range, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-1996-A, 4 sheets, scale 1:250,000, 22 p.
Nokleberg, W.J., Moll-Stalcup, E.J., Miller, T.P., Brew, D.A., Grantz, Arthur, Reed, J.C., Jr., Plafker, George, Moore, T.E., Silva, S.R., and Patton, William W., Jr., 1994, Tectonostratigraphic terrane and overlap assemblage map of Alaska: U.S. Geological Survey Open-File Report 94-194, 53 p., scale 1:2,500,000.
Richter, D.H., Singer, D.A., and Cox, D.P., 1975, Mineral resources map of the Nabesna quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-655-K, 1 sheet, scale l:250,000.
Singer, D.A.., 1986, Descriptive model of kuroko massive sulfide, in Cox, D.P., and Singer, D.A., eds., Mineral deposit models: U.S. Geological Survey Bulletin 1693, p. 189-190.
Singer, D. A., Csejtey, Bèla, Jr., and Miller, R.J., 1980, Map and discussion of the metalliferous and selected non-metalliferous mineral resources of Talkeetna Mountains quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-558-Q, 34 p., 1 sheet, scale 1:250,000.
Singer, D.A., and MacKevett, E.M., Jr., 1977, Mineral resources map of the McCarthy quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-773-C, l sheet, scale l:250,000.
Singer, D.A.., and Mosier, D.L., 1986, Grade and tonnage model of kuroko massive sulfide, in Cox, D.P., and Singer, D.A., eds., Mineral deposit models: U.S. Geological Survey Bulletin 1693, p. 190-197.

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