292 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Burns, L.E., 1985, The Border Ranges ultramafic and mafic complex, south-central <strong>Alaska</strong>—cumulate fractionates of island-arc volcanics: Canadian Journal of Earth Sciences, v. 22, p. 1020-1038. Butnerchuk, S.B., and Hancock, K.D., 1997, Barite in British Columbia: British Columbia Ministry of Energy and Mines Open File 1997, 145 p. Butrenchuk, S.B., 1991, Gypsum deposits in British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong>, Open File 1991-15. Butrenchuk, S.B., 1996, Phosphate deposits in British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> Bulletin 98, 126 p. Byalobzhesky, S.G., Korago, E.A., Lychagin, P.P., Kolyasnikov, Yu A., and Likman, V.B., 1990, South Anyui zone—Longlived development of folded structure, in Tectonics and metallogeny of U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, Magadan, p. 29-31 (in Russian). Byers, F.M., Jr., and Sainsbury, C.L., 1956, Tungsten deposits of the Hyder district, <strong>Alaska</strong>: U.S. Geological Survey Bulletin 1024-F, p. 123-140. Bysouth, G.D., and Wong, G.Y., 1995, The Endako molybdenum mine, central British Columbia—An update, in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America, Canadian Institute of Mining and Metallurgy Special <strong>Paper</strong> 46, p. 697-703. Cady, W.M., Wallace, R.E., Hoare, J.M., and Webber, E.J., 1955, The central Kuskokwim region, <strong>Alaska</strong>: U.S. Geological Survey <strong>Professional</strong> <strong>Paper</strong> 268, 132 p. Caira, N.M., Findlay, A., DeLong, C., and Rebagliati, C.M., 1995, Fish Lake porphyry copper-gold deposit, central British Columbia: in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining and Metallurgy Special Volume 46, p. 327-342. Cairnes, C.E., 1934, Slocan Mining Camp, British Columbia: Geological Survey of Canada Memoir 173, 137 p. Campbell, F.A., 1960, Nickel deposits in the Quill Creek and White River areas, Yukon: Canadian Institute of Mining and Metallurgy, Bulletin, v. 53, p. 953-959. Campbell, S.W., 1976, Nickel-copper sulphide deposits in the Kluane Ranges, Yukon Territory: Department of Indian and Northern Affairs Open-File Report EGS 1976-10, 17 p. Cant, D.J., 1989, Zuni sequence—the Foreland Basin, Lower Zuni sequence: Middle Jurassic to Middle Cretaceous, in Ricketts, B.D., ed., Western Canada sedimentary basin; a case history: Canadian Society of Petroleum Geologists, Calgary, p. 251-267. Carne, R.C., 1979, Upper Devonian barite-lead-zinc-silver mineralization at Tom claims, Macmillan Pass, Yukon Territory: Vancouver, University of British Columbia, M.S. thesis, 149 p. Carriere, J.J., Sinclair, W.D., and Kirkham, R.V., 1981, Copper deposits and occurrences in Yukon Territory: Geological Survey of Canada <strong>Paper</strong> 81-12, 62 p. Carson, D.J.T., 1973, The plutonic rocks of Vancouver Island: Geological Survey of Canada <strong>Paper</strong> 72-44, 70 p. Carson, D.J.T., and Jambor, J.L., 1974, Mineralogy, zonal relationships and ecomonic significance of hydrothermal alteration at porphyry copper deposits, Babine Lake area, British Columbia: Canadian Institute of Mining and Metallurgy Bulletin, v. 67, p. 110-133. Carson, D.J.T., Jambor, J.L., Ogryzlo, P., and Richards, T.A., 1976, Bell Copper—Geology, geochemistry and genesis of a supergene-enriched, biotitized porphyry copper deposit with a superimposed phyllic zone, in Brown, Sutherland, A., ed., Porphyry Deposits of the Canadian Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 15, p. 245-263. Carter, N.C., 1970, Len, in Geology, Exploration and Mining in British Columbia 1970: British Colmbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong>, p. 104-107. Carter, N.C., 1982, Porphyry copper, and molybdenum deposits, west-central British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong>, Bulletin 64, 150 p. Carter, N.C., Dirom, G.E., and Ogryzlo, P.L., 1995, Porphyry copper-gold deposits, Babine Lake area, west-central British Columbia, in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining, Metallurgy, and Petroleum Special Volume 46, p. 247-255. Casselman, M.M., McMillan, W.J., and Newman, K.M., 1995, Highland Valley porphyry copper deposits near Kamloops, Biritsh Columbia—A review and update with emphasis on the Valley deposit, in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining and Metallurgy, and Petroleum, Special Volume 46, p. 161-191. Cathcart, S.H., 1922, Metalliferous lodes in southern Seward Peninsula: U.S. Geological Survey Bulletin 722, p. 163-261. Cathro, M.S., 1990, Gold, silver and lead deposits of the Ketza River district, Yukon, preliminary results of field work, in Abbott, J.G., and Turner, R.J.W., eds., Mineral Deposits of the Northern Canadian Cordillera, Yukon-northeastern British Columbia, Fieldtrip Guidebook No. 14, 8 th Symposium International Association on Genesis of Ore Deposits (IAGOD): Geological Survey of Canada Open File 2169, p. 269-282.
Cecile, M.P., 1982, The lower Paleozoic Misty Creek embayment, Selwyn Basin, Yukon, and Northwest Territories: Geological Survey of Canada Bulletin, v. 335, 78 p. Chapman, R.M., 1945. Molybdenum prospect in the southern part of Kaiyuh Hills, <strong>Alaska</strong>. U.S. Geological Survey Press Release, 1 p. Chartrand, F.M., Brown, A.C. and Kirkham, R.V., 1989, Diagenesis, sulphides and metal zoning in the Redstone copper deposit, Northwest Territories: Geological Association of Canada, Special <strong>Paper</strong> 36, p. 189-206. Chekhov, A.D., 1982, Tectonics of the Talovka-Pekulney zone: Essays on tectonics of the Koryak Highlands: Nauka, Moscow, p. 70-106 (in Russian). Chipp, E.R., 1970, Geology and geochemistry of the Chandalar area, Brooks Range, <strong>Alaska</strong>: <strong>Alaska</strong> Division of Mines and Geology Geologic Report 42, 39 p. Christopher, P.A., 1975, Carmi-Beaverdell area (82E/6,11), in Geological Fieldwork 1975: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong>, p. 27-31. Church, B.N., 1971, Geology of the Owen Lake, Parrott Lakes, and Goosly Lake area, in Geology, Exploration and Mining in British Columbia 1970: British Columbia Department of Mines, and Petroleum <strong>Resources</strong>, p. 119-125. Church, B.N., 1973, Geology of the White Lake Basin: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> Bulletin 61,120 p. Church, B.N., 1986, Geological setting and mineralization in the Mount Attwood-Phoenix area of Greenwood mining camp: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong>, <strong>Paper</strong> 1986-2, 65 p. Church, 1995, B.N., 1995, Bridge River mining camp; geology and mineral deposits: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> Report 1990-3, 95 p. Churkin, Michael, Jr., Nokleberg, W.J., and Huie, Carl, 1979, Collision-deformed Paleozoic continental margin, western Brooks Range, <strong>Alaska</strong>: Geology, v. 7., no. 8, p. 379-383. Collier, A.J., Hess, F.L., Smith, P.S., and Brooks, A.H., 1908, The gold placers of parts of Seward Peninsula, <strong>Alaska</strong>, including the Nome, Council, Kougarok, Port Clarence, and Goodhope precincts: U.S. Geological Survey Bulletin 328, 343 p. Collins, J.A., and Smith, L., 1977, Genesis of cupriferous quartz arenite cycles in the Grinnell Formation (Spokane equivalent), Middle Proterozoic (Helikian) Belt-Purcell Supergroup, eastern Rocky Mountains, Canada: Bulletin of Canadian petroleum Geology, v. 25, p. 713-735. References Cited 293 Coney, P.J., Jones, D.L., and Monger, J.W.H., 1980, Cordilleran suspect terranes: Nature, v. 288, p. 329-333. Cook, D.B., Fujita, K., and McMullen, C.A., 1986, Presentday plate interactions in northeast Asia—North American, Russian, and Okhotsk plates: Journal of Geodynamics, v. 6, p. 33-51. Cooper, A.K., Scholl, D.W., and Marlow, M.S., 1992, Evidence for Cenozoic crustal extension in the Bering Sea region: Tectonics, v. 11, p. 719-731. Cowan, D.S., 1994, Alternative hypotheses for the mid-Cretaceous paleogeography of the western Cordillera: GSA Today, v. 4, no. 7, p. 181-186. Cowan, D.S., Brandon, M.T., and Garver, J.I., 1997, Geologic tests for large coastwise displacements—a critique illustrated by the Baja British Columbia controversy: American Journal of Science, v. 297, p. 117-173. Cox, D.P., 1993, Estimation of undiscovered deposits in quantitative mineral resource assessments––examples from Venezuela and Puerto Rico: Nonrenewable <strong>Resources</strong>, v. 2, no. 2, p. 82–91. Cox, D.P., Detra, D.E., and Detterman, D.L., 1981, Mineral resource maps of the Chignik and Sutwik Island quadrangles, <strong>Alaska</strong>: U.S. Geological Survey Miscellaneous Field Studies Map MF-1053-K, 2 sheets, scale 1:250,000. Cox, D.P., and Singer, D.A., eds., 1986, Mineral deposit models: U.S. Geological Survey Bulletin 1693, 379 p. Crowe, D.E., Nelson, S.W., Brown, P.E., Shanks, W.C., III, and Valley, J.W., 1992, Geology and geochemistry of volcanogenic massive sulfide deposits and related igneous rocks, Prince William Sound, south-central <strong>Alaska</strong>: Economic Geology, v. 87, p. 1722-1746. Crowley, J.L., 1997, U-Pb geochronologic constraints on the cover sequence of the Monashee Complex, Canadian Cordillera: Paleoproterozoic deposition on basement: Canadian Journal of Earth Sciences, v. 34, p. 1008-1022. Csejtey, B., Jr., Mullen, M.W., Cox, D.P., Gilbert, W.G., Yeend, W.E., Smith, T.E., Wahrhaftig, C., Craddock, C., Brewer, W.M., Sherwood, K.W., Hickman, R.G., Stricker, G.D., St. Aubin, D.R., and Goerz, K.J., III, 1986, Geology and geochronology of the Healy quadrangle, <strong>Alaska</strong>. U.S. Geological Survey Open-File Report 86-396, 92 p., 3 sheets, scale 1:250,000. Cyr, J.B., Pease, R.B., and Schroeter, T.G., 1984, Geology and mineralization at Equity Silver Mine: Economic Geology, v. 79, p. 947-968. Czamanske, G.K., and Calk, L.C., 1981, Mineralogical records of cumulus processes, Brady Glacier Ni-Cu deposits, southeastern <strong>Alaska</strong>: Mining Geology, v. 31, no. 168, p. 213-233.
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USGS Prepared in collaboration with
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U.S. Department of the Interior Gal
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iv Hart River SEDEX Zn-Cu-Ag Deposi
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vi Specific Events for Middle Throu
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viii Metallogenic Belts Formed Duri
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x Origin of and Tectonic Controls f
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xii Toodoggone Metallogenic Belt of
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xiv Slate Creek Serpentinite-Hosted
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xvi Left Omolon Belt of Porphyry Mo
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xviii Origin of and Tectonic Contro
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xx Chukotka Metallogenic Belt of Au
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xxii Plutonic Rocks Hosting East-Ce
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xxiv Skeena Metallogenic Belt of Po
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xxvi Bee Creek Porphyry Cu Deposit
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xxviii 36. Wellgreen gabbroic Ni-Cu
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xxx 87. Partizanskoe Pb-Zn skarn de
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Metallogenesis and Tectonics of the
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format (Nokleberg and others, 1996)
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logenesis of the region (1) subduct
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Subterrane—A fault-bounded unit w
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dilemma consists of two conflicting
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2 to 20 m thick. A related dolomite
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Lantarsky-Dzhugdzhur Metallogenic B
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Origin of and Tectonic Controls for
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Metallogenic Belts Formed During Pr
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as at Oz, Monster, and Tart, may al
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Monashee Metallogenic Belt of Sedim
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Clark Range Metallogenic Belt of Se
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in addition to the Fe deposits. Min
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study) consists of lenses, from 100
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Omulev Austrian Alps W Deposit The
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ock, including coarse clastic rock,
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lative metalliferous brines in a re
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Prince of Wales Island Metallogenic
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suite of deposits and host rocks ar
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margin of the North American Craton
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newly created terranes migrated int
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(Ryazantzeva and Shurko, 1992). The
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tonnes Au and an average grade of a
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mafic and felsic metavolcanic rocks
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intrusion from about 402 to 366 Ma
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Origin of and Tectonic Controls for
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mentary rocks of the Cambrian to De
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(Preto and Schiarizza, 1985; Schiar
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Origin of and Tectonic Controls for
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ate and clastic rocks and volcanicl
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(Nokleberg and others, 1994c, 1997c
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Berezovka River Metallogenic Belt o
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Origin of and Tectonic Controls for
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Finlayson Lake Metallogenic Belt of
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and barite in siliceous black turbi
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Windermere Creek (Western Gypsum) C
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(NX, DL, MY), Viliga (VL), and Zolo
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South of the main east-west-trendin
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ated subduction zone in the Wrangel
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icite-biotite-quartz bodies in frac
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Canada Cordillera. The granitoid ro
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Viliga (VL) passive continental-mar
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32; tables 3, 4) occurs along the n
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superterrane, consists mainly of ma
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ers, 1994c, 1997c). In southern Bri
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mental volcanic rocks of intermedia
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a resource of 34.3 million tonnes o
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potassic zone. Combined estimated p
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and quartz monzodiorite stock and s
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and Omolon (OM) cratonal terranes,
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in volcanic and volcaniclastic rock
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minor calcite, and sporadic pyrite
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supergene blanket are interpreted a
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deposits and occurrences consist of
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onto the Omulevka terrane to form t
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superterrane. This belt is interpre
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to form along the leading edge of t
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quartz, and is virtually not associ
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deposits are at Terrassnoe and Kuna
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Peschanka Porphyry Cu-Mo Deposit Th
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The belt is hosted in the Late Jura
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in a island arc that was tectonical
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and Early Cretaceous Koyukuk island
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The deposit consists of disseminate
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The Orange Hill deposit contains an
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49; tables 3, 4) (Foley and others,
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locally Late Triassic marine volcan
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gold in a gangue of quartz, calcite
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Verkhoyansk granite belt, which int
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metallogenic belts are interpreted
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assemblages, which may have been mo
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during hypogene and supergene alter
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collision and regional thrusting, t
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Yur Au Quartz Vein Deposit The smal
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phase has a Rb-Sr isotopic age of 1
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sian Northeast. The belt is hosted
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Host Granitoid Rocks and Associated
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that are up to 600-1,500 m long, av
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Metallogenic Belts Formed During La
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y partly coeval plutons that range
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tion is interpreted as occuring by
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the Badzhal-Ezop and Khingan parts
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and comagmatic with volcanic rocks;
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as interpreted for the Rock Creek d
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source (Yeo, 1992). The Blow River
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2000). The spatial location of the
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to the east in the central Yukon Te
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occur in a 30-km-long belt along ir
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The Emerald deposit has produced ap
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Metallogenic-Tectonic Model for Ear
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cham oceans were closed, and the Ch
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greisenized Mesozoic granite that i
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composition magmatic bodies (with a
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Origin of and Tectonic Controls for
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to Albian pelecypods (Nokleberg and
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quartz-arsenopyrite-pyrrhotite, pol
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thermally altered to siliceous and
- Page 227 and 228:
These ore bodies are as much as 1 m
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Eastern Asia-Arctic Metallogenic Be
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Demin, and Krasilnikov, 1974; Nekra
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10 percent Cu, as much as 0.92 perc
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pyrite, pyrite, galena, sphalerite,
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content decreases with depth, as do
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azdelnoye, (2) porphyry Sn deposits
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Karalveem Au Quartz Vein Deposit Th
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Democrat (Mitchell Lode) Granitoid-
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with high-temperature and high-pres
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chalcocite and covellite and also h
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cum-North Pacific, (2) completion o
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(6) In the Paleocene (about 56 to 6
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sists of cinnabar and metacinnabari
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Eastern Asia-Arctic Metallogenic Be
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groups of deposits are interpreted
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Indian Mountain and Purcell Mountai
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and southeastern Alaska (Moll and P
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Nokleberg and others, 1995a; Bundtz
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g/t Au or 368.2 Au gold. The deposi
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wim Group and altered mafic dikes.
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Mount Nansen porphyry Cu-Mo deposit
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A Map 450 500 550 Cross section Dik
- Page 273 and 274: Cretaceous and early Tertiary conti
- Page 275 and 276: deposits, at Chichagoff and Hirst-C
- Page 277 and 278: others, 1994c, 1997c). The signific
- Page 279 and 280: tonnes grading 0.53 percent Ni, 0.3
- Page 281 and 282: with a 0.25 percent cut-off. The de
- Page 283 and 284: Bulkley Metallogenic Belt of Porphy
- Page 285 and 286: Red Rose W-Au-Cu-Ag Polymetallic Ve
- Page 287 and 288: ish Columbia and consists of severa
- Page 289 and 290: during back-arc extension or transt
- Page 291 and 292: stocks and dikes, is associated wit
- Page 293 and 294: etrograde minnesotaite (Fe talc), F
- Page 295 and 296: Specific Events for Early to Middle
- Page 297 and 298: of fractured and faulted Permian-Tr
- Page 299 and 300: sists of a mineralized fracture zon
- Page 301 and 302: dolomite. Wall rock alteration incl
- Page 303 and 304: elt of late Tertiary plutons that a
- Page 305 and 306: plates that exhibit magnetic anomal
- Page 307 and 308: stages (Petrenko, 1999): (1) In the
- Page 309 and 310: mon. The deposit is of medium size
- Page 311 and 312: Metallogenic-Tectonic Model for Lat
- Page 313 and 314: The origin of the Hg deposits of th
- Page 315 and 316: margin or island-arc tectonic envir
- Page 317 and 318: Columbia: Implicatons for the Middl
- Page 319 and 320: Bazard, D.R., Butler, R.F., Gehrels
- Page 321 and 322: Bradley, D.C., Haeussler, P.J., and
- Page 323: Bundtzen, T.K., Laird, G.M., Caluti
- Page 327 and 328: Debari, S.M., and Coleman, R.G., 19
- Page 329 and 330: U.S. Bureau of Land Management Open
- Page 331 and 332: Cordilleran Orogen in Canada: Geolo
- Page 333 and 334: Goldfarb, R., Hart, C., Miller, M.,
- Page 335 and 336: Grove, E.W., 1986, Geology and mine
- Page 337 and 338: Høy, T., 1982a, Stratigraphic and
- Page 339 and 340: Jones, D.L., Silberling, N.J., Cone
- Page 341 and 342: Kutyev, F. Sh., Baikov, A.I., Sidor
- Page 343 and 344: Shield—Ultramafic magma and its m
- Page 345 and 346: Manns, F.T., 1981, Stratigraphic as
- Page 347 and 348: Miller, M.L., and Bundtzen, T.K., 1
- Page 349 and 350: Mortimer, N., 1987, The Nicola Grou
- Page 351 and 352: Noble, S.R., Spooner, E.T.C., and H
- Page 353 and 354: Canada Annual Meeting, Saskatoon, S
- Page 355 and 356: Perello, J.A., Fleming, J.A., O’K
- Page 357 and 358: Far East—Mineralogical criteria f
- Page 359 and 360: Roeske, S.M., Mattinson, J.M., and
- Page 361 and 362: Schmidt, J.M., and Zierenberg, R.A.
- Page 363 and 364: formation occurrences: Materialy po
- Page 365 and 366: Struik, L.C., 1986, Imbricated terr
- Page 367 and 368: Valuy, G., and Rostovsky, F., 1988,
- Page 369 and 370: Wolfe, W.J., 1995, Exploration and
- Page 371 and 372: Appendix Table 1. Mineral deposit m
- Page 373 and 374: Table 2 Summary of correlations and
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Table 2—Continued Unit(s) and Cor
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Table 2—Continued Unit(s) and Cor
- Page 379 and 380:
Table 3—Continued Metallogenic Be
- Page 381 and 382:
Table 3—Continued Metallogenic Be
- Page 383 and 384:
Table 3—Continued Metallogenic Be
- Page 385 and 386:
Table 3—Continued Metallogenic Be
- Page 387 and 388:
Table 3—Continued Metallogenic Be
- Page 389 and 390:
Table 3—Continued Metallogenic Be
- Page 391 and 392:
Table 3—Continued Metallogenic Be
- Page 393 and 394:
Table 3—Continued Metallogenic Be
- Page 395 and 396:
Table 3—Continued Metallogenic Be
- Page 397 and 398:
Table 3—Continued Metallogenic Be
- Page 399 and 400:
Table 4. Significant lode deposits,
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Table 4—Continued Appendix 369 De
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Table 4—Continued Tracy Metalloge
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Table 4—Continued Appendix 373 In
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Table 4—Continued Deposit Name Mi
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Table 4—Continued Mainits Metallo
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Table 4—Continued Deposit Name Mi
- Page 413 and 414:
Table 4—Continued Appendix 381 De
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Table 4—Continued Whitehorse Meta
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Table 4—Continued Deposit Name Mi
- Page 419 and 420:
Table 4—Continued Appendix 387 De
- Page 421 and 422:
Table 4—Continued Appendix 389 LA
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Table 4—Continued Deposit Name Mi
- Page 425 and 426:
Table 4—Continued Surprise Lake M
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Table 4—Continued Sredinny Metall
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Table 4—Continued Deposit Name Mi