310 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera tion in the Mutnovsky area, Kamchatka, Russia: Society of Economy Geology Newsletter, no. 20, p. 1, 6-9. Lawver, L.A., and Scotese, C.R., 1990, A review of tectonic models for the evolution of the Canada Basin, Chapter 31, in Grantz, A., Johnson, L., and Sweeny, J.F., eds., The Arctic Ocean region: Boulder, Colo., Geological Soceity of America, The Geology of North America, v. L., p. 593-618. Layer, P.W., Ivanov, V.V., and Bundtzen, T.K., 1994, 40 Ar/ 39 Ar ages from ore deposits in the Okhotsk-Chukotka belt, Northeast Russia [abs.]: International Conference on Arctic Margin (ICAM), Magadan, Russia, p. 50 (in Russian and English). Layer, P.W., Parfenov, L.M., Trunilina, V.A., and Bakharev, A.G., 1995, Age and tectonic signficance of granitic belts within the Verkhoyansk fold an thrust belt, Yakutia, Russia [abs.]: Geological Society of America Abstracts with Programs, v. 27, p. 60. Layne, G.D., and Spooner, E.T.C., 1986, The JC Sn-Fe-F skarn, Seagull Batholith area, southern Yukon, in Morin, J.A., ed., Mineral Deposits of the Northern Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 37, p. 266-273. Layne, G.D., and Spooner, E.T.C., 1986, The JC Sn-Fe-F slarn, Seagull Batholith area, southern Yukon: in Morin, J.A., ed., Mineral deposits of the Northern Cordillera, Canadian Institute of Mining and Metallurgy Special Volume 37, p. 266-273. Leaming, S.F., 1978, Jade in Canada: Geological Survey of Canada <strong>Paper</strong> 78-19, 59 p. Lebedev, G.S., Ivanenko, V.V., Korpenko, V.I., 1994, Geochronology of volcanic-plutonic complexes in the Verkhneurmi ore field: Geology of Ore Deposits, v. 36, p. 362-371. LeCouteur, P.C., 1979, Age of the Sullivan lead-zinc deposit, in Evolution of the Cratonic Margin and Related Mineral Deposits: Geological Association of Canada, Cordilleran Section Symposium, Program and Abstracts, p.19. LeCouteur, P.C. and Tempelman-Kluit, D. J., 1976, Rb/Sr ages and a profile of Sr 87 / Sr 86 ratios for plutonic rocks across the Yukon Crystalline Terrane; Canadian Journal of Earth Sciences, v. 13, p. 319-330. Lees, B.J., 1936, Geology of the Teslin-Quiet Lake area, Yukon: Geological Survey of Canada Memoir 203, p. 24-25. Lefebure, D.W., Brown, D.A., and Ray, G.E., 1998, The British Columbia sediment-hosted gold project, Geological Fieldwork – 1998: British Columbia Ministry of Energy and Mines <strong>Paper</strong> 1999-1, p. 165-178. Lefebure, D., and Cathro, M., 1999, Plutonic related goldquartz veins and their potential in British Columbia: Kamloops Exploration Group Short Course on Plutonic Related Gold, April 9, 1999, pp. 185-221. Leitch, C.H.B., 1991, Preliminary studies of fluid inclusions in barite from the Middle Valley sulphide mounds, northern Juan de Fuca Ridge, in Current Research, Part A: Geological Survey of Canada <strong>Paper</strong> 91-1A, p. 27-30. Leitch, C.H.B., Dawson, K.M., and Godwin, C.I., 1989, Early Late Cretaceous-early Tertiary gold mineralization—A galena lead isotopic study of the Bridge River mining camp, Southwestern British Columbia, Canada: Economic Geology, v. 84, p. 2226-2236. Leitch, C.H.B., and Turner, R.J.W., 1991, The vent complex of the Sullivan stratiform sediment hosted Zn-Pb deposit, British Columbia—Preliminary petrographic and fluid inclusion studies: in Current Research, Part E: Geological Survey of Canada <strong>Paper</strong> 91-1E, p. 33-44. Leitch, C.H.B., and Turner, R.J.W., 1992, Preliminary field and petrographic studies of the sulphide-bearing network underlying the western orebody, Sullivan stratiform sediment-hosted Zn-Pb deposit, British Columbia: in Current Research, Part E, Geological Survey of Canada <strong>Paper</strong> 92- 1E, p. 61-71. Leitch, C.H.B., Godwin, C.A., and Dawson, K.M., 1989, Early Late Cretaceous-early Tertiary gold mineralization, a galena lead isotope study of the Bridge River mining camp, southwestern British Columbia, Canada: Economic Geology, v. 84, p. 2226-2236. Leitch, C.H.B., Hood, C.T., Cheng, Xiao-lin, and Sinclair, A.J., 1990, Geology of the Silver Queen mine area, Owen Lake, central British Columbia, in Geological Fieldwork 1989: British Columbia Geological Survey Branch <strong>Paper</strong> 1990-1, p. 287-295. Leitch, C.H.B., Ross, K.V., Fleming, J.A., and Dawson, K.M., 1995, Preliminary studies of hydrothermal alteration events at Island Copper deposit, northern Vancouver Island, British Columbia: Geological Survey of Canada Current Research, 1995-A, p. 51-59. Leitch, C.H.B., van der Heyden, P., Godwin, C.I., Armstrong, R.L., and Harakal, J.E., 1991, Geochronometery of the Bridge River camp, southwestern British Columbia: Canadian Journal of Earth Sciences, v. 28, p. 195-208. Lennan, W.B., 1986, Ray Gulch tungsten skarn deposit, Dublin Gulch area, centnal Yukon; in Morin, J.A., ed., Mineral Deposits of the Northern Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 37, p. 245-254. Lennikov, A.M., 1979, Anothosites of the southern portion of the Aldan Shield and surrounding areas: Nauka, Moscow, 345 p. (in Russian). Lennikov, A.M., Oktyabrsky, R.A., and Avdevnina, L.A., 1987, Peculiarities of composition and genesis of Early Archean mafic-ultramafic intrusions of Southern Aldan
Shield—Ultramafic magma and its metallogeny: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, p. 93-118 (in Russian). Leriche, P.D., 1995, Taurus copper-molybdenum porphyry deposit, east-central <strong>Alaska</strong>, 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. 451-457. Light, T.D., Brew, D.A., and Ashley, R.P., 1989, The <strong>Alaska</strong>- Juneau and Treadwell lode gold systems, southeastern <strong>Alaska</strong>, in Shawe, D.R., Ashley, R.P., and Carter, L.M.H., eds., Gold deposits in metamorphic rocks-Part I: U.S. Geological Survey Bulletin 1857-D, p. D27-D36. Linnen, R.L., Williams-Jones, A.E., Leitch, C.H.B., and Macauley, T.N., 1995, Molybdenum mineralization in a fluorine-poor system: The Trout Lake stockwork deposit, southeastern 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. 771-780. Loney, R.A., and Himmelberg, G.R., 1984, Preliminary report on ophiolites in the Yuki River and Mount Hurst areas, west-central <strong>Alaska</strong>, in Coonrad, W.L., and Elliott, R.L., eds., The United States Geological Survey in <strong>Alaska</strong>— Accomplishments during 1981: U.S. Geological Survey Circular 868, p. 27-30. Loney, R.A., and Himmelberg, G.R., 1989, The Kanuti ophiolite, <strong>Alaska</strong>: Journal of Geophysical Research, v. 94, p. 15869-15900. Loney, R.A., and Himmelberg, G.R., 1992, Petrogenesis of the Pd-rich intrusion at Salt Chuck, Prince of Wales Island—an early Paleozoic <strong>Alaska</strong>n-type ultramafic body: Canadian Mineralogist, v. 30, p. 1004-1022. Loney, R.A., Himmelberg, G.R., and Shew, Nora, 1987, Salt Chuck palladium-bearing ultramafic body, Prince of Wales Island, in Hamilton, T.D., and Galloway, J.P., eds., Geologic studies in <strong>Alaska</strong> by the U.S. Geological Survey during 1986: U.S. Geological Survey Circular 998, p. 126-127. Lonsdale, P., 1988, Paleogene history of the Kula plate—offshore evidence and onshore implications: Geological Society of America Bulletin, v. 100, p. 755-766. Lowell, J.D., and Guilbert, J.M., 1970, Lateral and vertical alteration-mineral zoning in porphyry ore deposits: Economic Geology, v. 65, p. 373-408. Ludington, S., and Cox, D., 1996, Data base for a national mineral-resource assessment of undiscovered deposits of gold, silver, copper, lead, and zinc in the conterminous United States by U.S. Geological Survey Minerals Team: U.S. Geological Survey Open-File Report 96-96, 1 CD- ROM. References Cited 311 Lugov, S.F., ed., 1986, The Koryak Upland—A new tin-bearing area—the geology of the tin deposits of the U.S.S.R. Northeast: Nedra, Moscow, 101 p. (in Russian). Lugov, S.F., Makeev, B.V., and Potapova, T.M., 1972, Regularities of formation and distribution of tin deposits in the U.S.S.R. Northeast: Nedra, Moscow, 358 p (in Russian). Lugov, S.F., Podolsky, A.M., Speranskaya, I.M., and Titov, V.A., 1974a, Tin capacity of the Okhotsk-Chukotka volcanic belt: Nedra, Moscow, 183 p (in Russian). Lugov, S.F., Rozhkov, Yu. P., and Ivanov, A.A., 1974, The geological peculiarities of tin mineralization of the Koryak highlands and its perspectives: Geologiya Rudnykh Mestorozhdeniy, no. 3, p. 27-39 (in Russian). Lull, J.S., and Plafker, George, 1990, Geochemistry and paleotectonic implications of metabasaltic rocks in the Valdez Group, southern <strong>Alaska</strong>, in Dover, J.H., and Galloway, J.P., eds, Geological Studies in <strong>Alaska</strong> by the U.S. Geological Survey, 1989: U.S. Geological Survey Bulletin 1946, p. 29-38. Lychagin, P.P., 1967, Depth facies and relative temperature of formation of tin, polymetallic and gold-silver epithermal mineralization in the Kulu River basin—Ore capacity of volcanogenic formations in the U.S.S.R. Northeast and Far East: U.S.S.R. Academy of Sciences, Magadan, p. 88-93 (in Russian). Lychagin, P.P., 1985, The Aluchinsk Massif and the problem of ophiolite ultramafics and gabbroids in Mesozoic fold belts of the U.S.S.R. North East: Tikhookeanskaya Geologiya, no. 5, p. 33-41 (in Russian). Lychagin, P.P., Dylevsky, E.F., Shpikerman, V.I., and Likman, V.B., 1989, Magmatism of central regions of the U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, 120 p (in Russian). Lydon, J.W., 1995, The Sulivan deposit and its geological environment—The Sullivan Project; Geological Association of Canada Mineral Deposits Division Newsletter, The Gangue, issue 49, July, 1995, p.15-17. Lynch, J.V.G., 1989, Large-scale hydrothermal zoning reflected in the tetrahedrite-freibergite solid solution, Keno Hill Ag-Pb- Zn district, Yukon: Canadian Mineralogist, v. 27, p. 383-400. Lytwyn, J., Casey, J., and Gilbert, S., 1997, Arc-like mid-ocean ridge basalt formed seaward of a trench-fore-arc system just prior to ridge subduction—an example from subaccreted ophiolites in southern <strong>Alaska</strong>: Journal of Geophysical Research, v. 102, no. B5, p. 10225-10242. Macauley, T.N., 1973, Geology of the Ingerbelle and Copper Mountain deposits at Princeton, British Columbia: Canadian Institute of Mining and Metallurgy, Bulletin, v. 66, no. 732, p. 105-112.
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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
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during back-arc extension or transt
- Page 291 and 292: stocks and dikes, is associated wit
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- 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
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- 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: Kutyev, F. Sh., Baikov, A.I., Sidor
- 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
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- Page 393 and 394:
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 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
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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