308 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Kirkham, R.V., 1974, A synopsis of Canadian stratiform copper deposits in sedimentary sequences: Centenaire de la Societe Geologique de Belgique, Gisements Stratiformes et Provinces Cupriferes, Liege, p. 367-382. Kirkham, R.V., 1996a, Sediment-hosted stratiform copper; in Eckstrand, O.R., Sinclair, W.D., and Thorpe, R.I., eds., Geology of Canadian Mineral Deposit Types, Geological Survey of Canada, Geolology of Canada, no. 8, p. 223-240. Kirkham, R.V., 1996b, Volcanic redbed copper, in Eckstrand, O.R., Sinclair, W.D., and Thorpe, R.F., eds., Geology of Canadian mineral deposit types: Geological Society of America, The Geology of North America, v. F-1, p. 473- 483. Kirkham, R.V., and Margolis, J., 1995, Overview of the Sulphurets area, northwestern British Columbia, 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. 473-483. Klimov, N.V., 1979, Mercury, in Arkhipov, Yu.V. and Frumkin, I.M., eds., Geology of U.S.S.R., Minerals of Yakutia: Nedra, Moscow, v. 18, p. 249-259 (in Russian). Kolyasnikov, Yu. A., and Kulish, L.I., 1988, Manganese metamorphic concentrations in volcanic-sedimentary rocks of the Anadyr-Koryak fold belt: Metamorphogenic ore formation of low-grade facies metamorphism in Phanerozoic fold belt: Nauka, Kiev, p. 185-193 (in Russian). Konstantinov, M.M., Natalenko, V.E., Kalinin, A.I., Strujkov, S.F., 1998, Ducat gold-silver deposit: Nedra Publisher House, Moscow, 203 p. Konstantinovskaya, E.A., 1999 Geodyamics of island arc-continent collison in the western Pacific margin: Geotectonics, v. 33, p. 15-34. Konyshev, V .O., Zhidkov, N.A., and Stepanov, V.A., 1993, Gold mercury deposits in Yakutia: Kolyma, v. 3, p. 11-15 (in Russian). Kopytin, V.I., 1978, Volcanic-hosted mercury mineralization in Chukotka—Mercury mineralization in orogenic volcanic complexes of the U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, p. 50-119 (in Russian). Korostelev, P.G., Gonevchuk, V.G., Gonevchuk, G.A., and others, 1990, Mineral assemblages of a greisen tungsten-tin deposit (Primorye), in Gvozdev, V.I., ed., Mineral assemblages of tin and tungsten deposits in the Russian Far East: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, p. 17-61 (in Russian). Koski, Randolph A; Silberman, M L; Nelson, S W; Dumoulin, J A., 1985, Rua Cove; anatomy of volcanogenic Fe-Cu sulfide deposit in ophiolite on Knight Island, <strong>Alaska</strong> [abs]: American Association of Petroleum Geologists Bulletin 69, p. 667. Korostylyov V.I., 1982, The geology and tectonics of the Southern Verkhoyan area: Nauka, Novosibirsk, 217 p. (in Russian). Kozin, N.N., Loginov, V.A., Kozlov, A.P., Zaitsev, V.P., and Sidorov, E.G., 1999, The platinum mining activities of Koryak Geology Mining Company in Northern Kamchatka, in Schafer, Robert, and Bundtzen, T.K., eds., Session on the Mineral Current Developments in the Russian Far East: Proceedings of the Prospectors and Developers Association of Canada, Toronto, Ontario, p. 247-251. Koz’min, B.M., 1984, Seismic belts of Yakutia and the mechanisms of their earthquakes: Nauka, Moscow, 125 p. (in Russian). Koz’min, B.M., Imaev, V.S., Imaeva, L.P., Fujita, K., Chung, W.Y., and Gao, H., 1996, Seismicity and active faults of the eastern Siberian platform [abs.]: Eos, Transactions, American Geophysical Union, v. 15, p. F521 Kozlovsky, E.A., ed., 1988, Geology of the BAM Zone, geological structure: Nedra, Leningrad, 443 p. (in Russian). Krasilnikov, A.A., Leibova, L.M., Khrustakeva, L.B., Nekrasova, A.N., Krasilnikova, L.N., and Demin, G.P., 1971, Geologic-structural peculiarities and mineral composition of hydrothermally altered rocks and ore bodies of the Karamken gold-silver deposit [abs.], in Metallogenic Specialization of Volcanic Belts and Volcano-Tectonic Structures in the Far East and Other Regions of the U.S.S.R.: U.S.S.R. Academy of Sciences, Vladivostok, p. 36-39 (in Russian). Krasny, L.I., and Rasskasov, Yu.P., 1975, The new ore district in the northern Priokhotye: Geologiya i Razvedka, v. 12, p. 5-11 (in Russian). Kuleshov, B.A., Pristavko, V.A., and Plyashkevich, A.A., 1988, Geological-structural and mineralogical-geochemical peculiarities of the Svetly tin-tungsten deposit (Chukotka): Tikhookeanskaya Geologiya, no. 4, p. 65-76 (in Russian). Kusky, T.M., Bradley, D.C., Haeussler, P.J., and Karl, S. 1997, Controls on accretion of flysch and melange belts at convergent margins: evidence from the Chugach Bay thrust and Iceworm melange, Chugach accretionary wedge, <strong>Alaska</strong>: Tectonics, v. 16, p. 855-878. Kusky, T.M., and Young, C.P., 1999, Emplacement of the Resurrection Peninsula ophiolite in the southern <strong>Alaska</strong> fore-arc during a ridge-trench encounter: Journal of Geophysical Research, v.104, p.29025-29054. Kutyev, F. Sh., Baikov, A.I., and Sidorov, E.G., 1988a, Platinum ore formations of the Koryak-Kamchatka region [abs.], in Ore Formations in Zone of Continent-to-Ocean Transition: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, v. 1, p. 115- 116 (in Russian).
Kutyev, F. Sh., Baikov, A.I., Sidorov, E.G., Semenov, V.L., Reznichenko, V.S., Simonova, L.S., and Kutyeva, G.V., 1988b, Metallogeny of Mafic-ultramafic complexes of the Koryak-Kamchatka region [abs.], in Magmatism and ore capacity of volcanic belts: U.S.S.R. Academy of Sciences, Khabarovsk, p. 73-74 (in Russian). Kutyev, F. Sh., Sidorov, E.G., Reznichenko, V.S., and Semenov, V.L., 1991, New data on platinoids in zonal ultramafic massifs of southern Koryak Upland: U.S.S.R. Academy of Sciences Reports, 317, no. 6, p. 1458-1461 (in Russian). Kutyrev, E.I., 1984, Geology and prediction of conformable copper, lead and zinc deposits, Nedra, Leningrad, 248 p. (in Russian). Kutyrev, E.I., Mikhailov, B.M., and Lyakhnitsky, Yu.S, 1989, Karst deposits: Nedra, Leningrad, 311 p. (in Russian). Kutyrev, E.I., Sobolev, A.E., Isparavnikov, A.V., Tolstyh, A.N., and Shleikin, P.D., 1988, Cupreous sandstones and cupreous basalts of the Sette-Daban area—Stratiforn mineralization in Yakutia: U.S.S.R. Academy of Sciences, Siberian Branch, Institute of Geology, Yakutsk, p. 74-86 (in Russian). Kutyrev, E.I., Sobolev, A.E., Tolstyh, A.N., and Shleikin, P.D., 1986, Cupreous sandstones and cupreous basalts in the southern Bilyakchan zone: Geologiya i Razvedka, no. 11, p. 11-13 (in Russian). Kuznetsov, V.A. and Yanshin, A.L., 1979, Stratiform lead-zinc deposits in Vendian sequences of the southeastern Yakutia: Nauka, Novosibirsk, 206 p. (in Russian). Lane, L.S., 1994; A new plate kinematic model of Canada Basin evolution, in Thurston, D., and Fujita, K., eds., Proceedings of 1994 International Conference on Arctic Margins: U.S. Department of Interior, Minerals Management Service, Anchorage, p. 283-288. Lane, L.S., 1997, Canada Basin, Arctic Ocean: evidence against a rotational origin: Tectonics, v. 16, p. 363-387 Lane, R.A., and Schroeter, T.G., 1995, Mineral occurrence investigations and exploration monitoring in the Nechako Plateau (93F/2,3,7,10,11,12,14,15 and 93C/9 and 16), in Geological Fieldwork 1994: British Columbia Geological Survey Branch, <strong>Paper</strong> 1995-1, p. 177- 191. Lang, J.R., Baker, Tim, Hart, Craig, and Mortensen, J.K., 2000, An exploration model for intrusion-related gold systems: Society of Economic Geologists (SEG) Newsletter, no. 40, p. 1; 6-15. Lange, I.M., and Nokleberg, W.J., 1984, Massive sulfide deposits of the Jarvis Creek terrane, Mt. Hayes quadrangle, eastern <strong>Alaska</strong> Range, <strong>Alaska</strong> [abs.]: Geological Society of America Abstracts with Programs, v. 16, p. 294. References Cited 309 Lange, I.M., Herberger, D., Whipple, J.W., and Krouse, H.R., 1989, Stratabound Cu-Ag and Pb-Zn mineralization, in Boyle, R.W., Brown, A.C., Jefferson, C.W., Jowett, E.C. and Kirkham, R.V., eds., Sediment-hosted stratiform copper deposits: Geological Association of Canada Special <strong>Paper</strong> 36, p. 287-304. Lange, I.M., Nokleberg, W.J., and Zehner, R.E., 1981, Mineralization of late Paleozoic island arc rocks of Wrangellia terrane, Mount Hayes quadrangle, eastern <strong>Alaska</strong> Range, <strong>Alaska</strong> [abs.]: Geological Association of Canada National Meeting Abstracts, v. 6, p. A-33. Lange, I.M., Nokleberg, W.J., Newkirk, S.R., Aleinikoff, J.N., Church, S.E., and Krouse, H.R., 1990, Metallogenesis of Devonian volcanogenic massive sulfide deposits and occurrences, southern Yukon-Tanana terrane, eastern <strong>Alaska</strong> Range, <strong>Alaska</strong>: Proceedings of the Pacific Rim 90 Congress, Australian Institute of Mining and Metallurgy, p. 443-450. Lange, I.M., Nokleberg, W.J., Newkirk, S.R., Aleinikoff, J.N., Church, S.E., and Krouse, H.R., 1993, Devonian volcanogenic massive sulfide deposits and occurrences, southern Yukon-Tanana terrane, eastern <strong>Alaska</strong> Range, <strong>Alaska</strong>: Economic Geology, v. 88, p. 344-376. Lange, I.M., Nokleberg, W.J., Plahuta, J.T., Krouse, H.R., and Doe, B.R., 1985, Geologic setting, petrology, and geochemistry of stratiform zinc-lead-barium deposits, Red Dog Creek and Drenchwater Creek areas, northwestern Brooks Range, <strong>Alaska</strong>: Economic Geology, v. 80, p. 1896-1926. Lanphere, M.A., and Reed, B.L., 1985, The McKinley sequence of granitic rocks—A key element in the accretionary history of southern <strong>Alaska</strong>: Journal of Geophysical Research, v. 90, p. 11413-11430. Large, D.E., 1983, Sediment-hosted massive sulphide lead-zinc deposits—An empirical model, in Sangster, D.F., ed., Short course in sediment-hosted stratiform lead-zinc deposits: Mineralogical Association of Canada, Handbook, v. 9, p.1-29. Larson, K.M., Freymueller, J.T., and Philipsen, S., 1997, Global plate velocities from the Global Positioning System: Journal of Geophysical Research, v. 102, no. B, p. 9961- 9981. Lashtabeg, V.I., Lugov, S.F., and Pozdeev, A.L., 1987, The Koryakskaya tin province: Sovietskaya Geologiya, no. 10, p. 54-59 (in Russian). Lassiter, J.C., DePaolo, D.J., and Mahoney, J.J., 1994, Geochemistry of the Wrangellia flood basalt province: Implications for the role of continental and oceanic lithosphere in flood basalt genesis: Journal of Petrology, v. 36, p. 983- 1010 Lattanzi, P., Okrugin, V.M., Corsini, F., Ignatiev, A., Okrugina, A., Tchubarov, V., and Livi, S., 1995, Geology, mineralogy, and geochemistry of base and precious metal mineraliza-
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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
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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
- 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 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: Jones, D.L., Silberling, N.J., Cone
- 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
- 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
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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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
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Table 4—Continued Appendix 387 De
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Table 4—Continued Appendix 389 LA
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Table 4—Continued Deposit Name Mi
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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