316 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Plafker, George, and Berg, H.C., eds., The geology of <strong>Alaska</strong>: Boulder, Colo., Geological Society of America: The Geology of North America, v. G-1, pl. 5, scale 1:2,500,000. Monger, J.W.H., and Berg, H.C., 1984, Lithotectonic terrane map of western Canada and southeastern <strong>Alaska</strong>, in Silberling, N.J., and Jones, D.L., eds., Lithotectonic terrane maps of the North American Cordillera: U.S. Geological Survey Open-File Report 84-523, p. B1-B31, 1 sheet, scale 1:2,500,000. Monger, J.W.H., and Berg, H.C., 1987, Lithotectonic terrane map of western Canada and southeastern <strong>Alaska</strong>: U. S. Geological Survey Miscellaneous Field Studies Map MF-1874- B, 1 sheet, scale 1:2,500,000, 12 p. Monger, J.W.H., and Nokleberg, W.J., 1996, Evolution of the northern North American Cordillera: Generation, fragmentation, displacement, and accretion of successive North American plate margin arcs, in Coyner, A.R., and Fahey, P.L., eds., Geology and Ore Deposits of the American Cordillera: Geological Society of Nevada Symposium Proceedings, Reno/Sparks, April 1995, p. 1133-1152. Monger, J.W.H., and Ross, C.A., 1971. Distribution of fusulinaceans in the Canadian Cordillera. Canadian Journal of Earth Sciences, v. 8, p. 770-791. Monger, J.W.H., Souther, J.G., and Gabrielse, H., 1972, Evolution of the Canadian Cordillera: a plate-tectonic model: American Journal of Science, v. 272, p. 577-602. Monger, J.W.H., van der Heyden, P., Journeay, J.M., Evenchick, C.A., and Mahoney, J.B., 1994, Jura-Cretaceous basins along the Canadian Cordillera: their bearing on pre-mid-Cretaceous sinistral displacements: Geology, v. 22, p. 175-178. Monger, J.W.H., Wheeler, J.O., Tipper, H.W., Gabrielse, H., Harms, T., Struik, L.C., Campbell, R.B., Dodds, C.J., Gehrels, G.E., and O’Brien, J., 1991, Part B, Cordilleran Terranes in Upper Devonian to Middle Jurassic assemblages, in Gabrielse, H., and Yorath, C.J., eds., Geology of the Cordilleran Orogen: Boulder, Colorado, Geological Society of America, The Geology of North America, v. G-2, p. 281-328. Moore, D.W., Young, L.E., Modene, J.S., and Plahuta, J.T., 1986, Geologic setting and genesis of the Red Dog zinclead-silver deposit, western Brooks Range, <strong>Alaska</strong>: Economic Geology, v. 81, p. 1696-1727. Moore, T.E., 1992, The Arctic <strong>Alaska</strong> superterrane, in Bradley, D.C., and Dusel-Bacon, Cynthia, eds., Geologic studies in <strong>Alaska</strong> by the U.S. Geological Survey, 1991: U.S. Geological Survey Bulletin 2041, p. 238-244 Moore, T.E., Wallace, W.K., Bird, K.J., Karl, S.M., Mull, C.G., and Dillon, J.T., 1992, Stratigraphy, structure, and geologic synthesis of northern <strong>Alaska</strong>: U.S. Geological Survey Open- File Report 92-330, 283 p, 1 plate. Moore, T.E., Wallace, W.K., Bird, K.J., Karl, S.M., Mull, C.G., and Dillon, J.T., 1994, Geology of northern <strong>Alaska</strong>, in Plafker, George, and Berg, H.C., eds., The Geology of <strong>Alaska</strong>: Boulder, Colorado, Geological Society of America, The Geology of North America, v. G-1, p. 49-140. Moores, E.M., 1991, Southwest U.S.-East Antarctic (SWEAT) connection—A hypothesis: Geology, v. 19, p. 425-428. Morganti, J.M., 1981, Ore deposit models—4. Sedimentarytype strataform ore deposits; some models amd a new classification: Geoscience Canada, v. 8, p. 65-75. Morin, J.A., 1978, A preliminary report on Hart River (116A/10)—-A Proterozoic massive sulphide deposit, in Mineral Industry Report 1977, Yukon Territory, EGS 1978- 79: Indian and Northern Affairs Canada, p. 22-25. Morin, J.A., 1981, The McMillan deposit—a stratabound lead-zinc-silver deposit in sedimentary rocks of Upper Proterozoic age, in Yukon Geology and Exploration 1979-80: Department of Indian and Northern Affairs, p. 105-109. Morrow, D.W., 1984, Sedimentation in Root Basin and Prairie Creek Embayment-Siluro-Devonian, Northwest Territories: Bulletin of Canadian Petroleum Geology, v.32, p. 162-189. Morrison, G.W., 1981, Setting and origin of skarn deposits in the Whitehorse Copper Belt, Yukon: London, Ontario, University of Western Ontario, Ph.D. dissertation, 306 p. Mortensen, J.K., 1992, Pre-mid-Mesozoic tectonic evolution of the Yukon-Tanana Terrane, Yukon and <strong>Alaska</strong>: Tectonics, v. 11, p. 836-853. Mortensen, J.K., Hart, C.J.R., Murphy, D.C., and Hefferman, S., 2000, Temporal evolution of early and mid-Cretaceous magmatism in the Tintina gold belt, in Tucker, T.L., and Smith, M.T., eds., The Tintina gold belt—Concepts, Exploration, and Discoveries: British Columbia and Yukon Chamber of Mines, Vancouver, Special Volume 2, p. 49-57. Mortensen, J.K., and Hulbert, L.J., 1991, A U-Pb age for the Maple Creek gabbro sill, Tatmagouche Creek area, southest Yukon Territory, in Radiogenic age and isotope studies, Report 5: Geological Survey of Canada <strong>Paper</strong> 91-2, p. 175-179. Mortensen, J.K., Johnston, S.T., Murphy, D.J., and Bremner, T.J., 1994, Age and metallogeny of Mesozoic and Tertiary plutonic suites in the Yukon [abs.], in Jambor, J.L., ed., Recent Developments in Yukon Metallogeny: Canadian Institute of Mining and Metallurgy 1994 Annual General Meeting, Abstracts and Proceedings, p. 45-47. Mortensen, J.K., and Thompson, R.I., 1990, A U-Pb zirconbaddeleyite age for a differentiated mafic sill in the Ogilvie Mountains, west-central Yukon Territory, in Radiogenic Age and Isotopic Studies, Report 3: Geological Survey of Canada <strong>Paper</strong> 1989-2, p. 23-28.
Mortimer, N., 1987, The Nicola Group—Late Triassic and early Jurassic subduction-related volcanism in British Columbia: Canadian Journal of Earth Sciences, v. 24, p. 2521-2536. Morton, R.D., Goble, R.J., and Fritz, P., 1974, The mineralogy, sulphur-isotope composition and origin of some copper dposits in the Belt Supergroup, southwest Alberta, Canada: Mineralium Deposita, v. 9, p. 223-241. Mull, C.G., Tailleur, I.L., Mayfield, C.F., Ellersieck, Inyo, and Curtis, Steven, 1982, New upper Paleozoic and lower Mesozoic stratigraphic units, central and western Brooks Range, <strong>Alaska</strong>: American Association of Petroleum Geologists Bulletin, v. 66, no. 3., p. 348-362. Mullen, A.W., 1984, Managing exploration and development programs for a variety of resource companies: Western Miner, v. 57, no. 4., p. 35-36. Muller, J.E., 1980, The Paleozoic Sicker Group of Vancouver Island, British Columbia: Geological Survey of Canada <strong>Paper</strong> 79-30, 24 p. Muller, J.E., and Carson, D.J.T., 1969, Geology and mneral deposits of Alberni map-area, British Columbia (92F): Geological Survey of Canada, Memoir 340, 137 p. Mulligan, R., 1984, Geology of Canadian tungsten occurrences: Geological Survey of Canada, Economic Geology Report 32, 121 p. Murphy, D.C., and Piercey, S.J., 1999, Finlayson Lake district—Geological evolution of Yukon-Tanana terrane and it’s implications to the Campbell Range belt, southeast Yukon: Yukon Exploration and Geology—1998: Exploration and Geological Serivces Division, Indian and Northern Affairs Canada, p. 47-63. Murphy, D.C. and Roots, C.F., 1992, Geology of Keno Hill, map area (105M/14) Yukon: Exploration and Geological Services Division, Indian and Northern Affairs Canada, Open File Map 1992-3, scale 1:50,000. Mustard, P.F., Roots, C.F., and Donaldson, J.A., 1990, Stratigraphy of the middle Proterozoic Gillespie Lake Group in the southern Wernecke Mountains, Yukon; geological Survey of Canada <strong>Paper</strong> 90-1E, p. 43-53. Natalenko, V.E., and Kalinin, A.I., 1991, Geological exploration for silver in the Dukat ore district: Kolyma, no. 7, p. 6-10 (in Russian). Natalenko, V.E., Kalinin, A.I., Raevskaya, I.S., Tolstikhin, Yu.V., Khalkhalov, Yu. A., and Belkov, E.V., 1980, Geologic structure of the Dukat deposit: Materialy po Geologii i Polzenym Iskopaemym Severo-Vostoka SSSR, U.S.S.R. Academy of Sciences, v. 25, p. 61-73 (in Russian). Natal’in, B.A., 1991, Mesozoic accretionary and collisional tectonics of the southern Far East: Tikhookeanskaya Geologiya, no. 5. (in Russian). References Cited 317 Natal’in, B.A., 1993, History and mode of Mesozoic accretion in southeastern Russia: The Island Arc, v. 2, p. 32-48. Natapov L.M., and Shuligina W.S., eds., 1991, Geologic map of the U.S.S.R.: U.S.S.R. Ministry of Geology, Leningrad, scale 1:1,000,000, 111 p., (in Russian). Nauman, C.R., Blakestad, R.A., Chipp, E.R., and Hoffman, B.L., 1980, The north flank of the <strong>Alaska</strong> Range, a newly discovered volcanogenic massive sulfide belt: Geological Association of Canada Program with Abstracts, p. 73. Nazarova, A.S., 1983, Ores of sulfide-cassiterite deposits as a promising source of combined commodities: Nedra, Moscow, 94 p. (in Russian). Nechaev, V.P., Markevich, P.V., Malinovsky, A.I., Philippov, A.N., and Vysotsky, S.V., 1996, Tectonic setting of the Cretaceous sediments in the Lower Amur Region, Russian Far East: Journal of Sedimentary Society of Japan, v. 43, p. 69-81. Neimark, L.A., Larin, A.M., Ovchinnikova, G.V., and Yakovleva, S.Z., 1992, Uranium-lead ages of the Dzhugdzhur anorthosites: Report of U.S.S.R. Academy of Sciences, v. 323, p. 514-518 (in Russian). Nekrasov, I.Ya., 1959, The occurrence of gold in the northwestern Verkhoyansk-Kolyma fold belt: U.S.S.R. Academy of Sciences, Siberian Branch, Institute of Geology, Yakutsk, no. 2, p. 10-16 (in Russian). Nekrasov, I.Ya., 1962, Magmatism and mineralization in the northwestern Verkhoyansk-Chukchi fold belt: Izvestiya Akademii Nauk, SSSR, Seriya Geologicheskaya, 335 p. (in Russian). Nekrasov, I.Ya., 1995, Genetic types of rare earth element (REE) mineralization in the Russian Far East, in Bundtzen, T.K., Fonseca, A.L., and Mann, Roberta, eds., The Geology and Mineral Deposits of the Russian Far East: <strong>Alaska</strong> Miners Association, Glacier House Publications, Anchorage, <strong>Alaska</strong>, p. 96-102. Nekrasov, I.Ya., Gamyanin, G.N., Goryachev, N.A., Zhdanov, Yu.Ya., Leskova, N.V., and Goryacheva, Ye.M., 1987, Mineralogy and geochemistry of silver mineralization in the Verkhoyansk-Kolyma fold belt—Silver antimony and goldsilver, mineral assemblages: Mineralogic Journal, no. 9, v. 6, p. 5-17 (in Russian). Nekrasov, I.Ya., and Korzhinskaya, V.S., 1991, New genetic type of tungsten-zirconium mineralization: Mineralogic Journal, v.13, p. 7-17 (in Russian). Nekrasov, I.Ya., and Pokrovsky, V.K., 1973, Tin-bearing properties of subvolcanic rocks in the northern portion of the Polousny Range and Primorskaya lowland, in Apeltsyn, F.E., Grinberg, G.A., Nekrasov, I.Ya., and Rubick , K.N., eds., Magmatism in the northeastern U.S.S.R.: Nauka, Moscow, p. 178-179 (in Russian).
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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
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Cretaceous and early Tertiary conti
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deposits, at Chichagoff and Hirst-C
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others, 1994c, 1997c). The signific
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tonnes grading 0.53 percent Ni, 0.3
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with a 0.25 percent cut-off. The de
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Bulkley Metallogenic Belt of Porphy
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Red Rose W-Au-Cu-Ag Polymetallic Ve
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ish Columbia and consists of severa
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during back-arc extension or transt
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stocks and dikes, is associated wit
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etrograde minnesotaite (Fe talc), F
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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 and 324: Bundtzen, T.K., Laird, G.M., Caluti
- Page 325 and 326: Cecile, M.P., 1982, The lower Paleo
- 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: Miller, M.L., and Bundtzen, T.K., 1
- 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
- Page 375 and 376: Table 2—Continued Unit(s) and Cor
- Page 377 and 378: 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
- Page 409 and 410:
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
- Page 423 and 424:
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