284 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera References Cited Abbott, G., 1981, A new geological map of Mt. Hundere and the area north, in Yukon Exploration and Geology 1979- 80: Department of Indian and Northern Affairs, Canada, p. 45-50. Abbott, J.G., 1983, Origin of the Clinton Creek asbestos deposit—Yukon Geology and Exploration, 1982: Department of Indian and Northern Affairs, Canada, p.18-25. Abbott, J.G., 1986a, Epigenetic mineral deposits of the Ketza- Seagull district, Yukon; in Yukon Geology, vol. 1: Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 56-66. Abbott, J.G., 1986b, Devonian extension and wrench tectonics near Macmillan Pass, Yukon territory, Canada; in Turner, R.W., and Einaudi, M.Y., eds., The Genesis of Stratiform Hosted Lead and Zinc Deposits, Conference Proceedings: Stanford University Press, p. 85-89 Abbott, J.G., Thorkelson, D.J. and Wallace, C.A., 1994, Regional setting of syngenetic, epigenetic and breccia- hosted precious and base-metal occurrences in Paleozoic and Proterozoic strata of Mackenzie Platform [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. 19-23. Abel, V.E., and Slezko, V.A., 1988, Stratiform gold mineralization of the Kharaulak anticlinorium, in Yakovlev, Ya.V., Davydov, Yu.V., and Kutyrev, E.I., eds., Stratiform mineralization in Yakutia: U.S.S.R. Academy of Sciences, Siberian Branch, Institute of Geology, Yakutsk, p. 110-117 (in Russian). Adams, D.D., Freeman, C.J., Goldfarb, R.J., Gent, C.A., and Snee, L.W., 1992, Age and geochemical constraints on mesothermal gold mineralization [abs.]: Geological Society of America Abstracts with programs, v. 24, p. 2. Aitken, J.D., 1991, Two late Proterozoic glaciations, Mackenzie Mountains, northwestern Canada: Geology, v. 19, no.5, p.445-448. Aitken, J.D., and McMechan, M.E., 1991, Middle Proterozoic 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. 97-124. Aksenova, V.D., Dovgal, Yu. M., and Sterligova, V.E., 1970, Nickel-chrome mineralization of Aluchin hyperbasite intrusion: Geologiya i Geofizika, no. 2, p. 23-33 (in Russian). Albers, J.P., Fraticelli, L.A., and Dawson, K.A., 1988, Metallogenic maps of the northeast quadrant of the Circum- Pacific region, showing inferred mineral belts and distribu- tion of oil and gas fields in accreted terranes and craton: U.S. Geological Survey Mineral Investigations Resource Map MR-95, 1 sheet, scale 1:20,000,000. Alldrick, Dani J.; Friedman, R.M., and Childe, F.C., 2001, Age and geologic history of the Ecstall greenstone belt, Northwest British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> Report: 2001-1, p. 269-278. Aleinikoff, J.N., Dusel-Bacon, C., Foster, H.L., and Nokleberg, W.J., 1987, Pb-isotope fingerprinting of tectonostratigraphic terranes, east-central <strong>Alaska</strong>: Canadian Journal of Earth Sciences, v. 24, p. 2089-2098. Aleinikoff, J.N., and Nokleberg, W.J., 1985, Age of Devonian igneous arc terranes in the northern Mount Hayes quadrangle, eastern <strong>Alaska</strong> Range, <strong>Alaska</strong>, in Bartsch-Winkler, Susan, ed., The United States Geological Survey in <strong>Alaska</strong>—Accomplishments during 1984: U.S. Geological Survey Circular 967, p. 44-49. Alekseenko, A.V., Korobeinikov, S.V., and Sidorov, V.A., 1990, New evidence of porphyry copper-molybdenum mineralization in Omolon massif—Ore formations of the U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, North- Eastern Interdisciplinary Research Institute, Magadan, p. 157-162 (in Russian). Alldrick, D.J., 1985, Stratigraphy and petrology of the Stewart mining camp (104B/1), in Geological Fieldwork 1984: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1985-1, p. 316-341. Alldrick, D.J., Brown, D.A., Harakal, J.E., Mortensen, J.K., and Armstrond, R.L., 1987, Geochronology of the Stewart Mining Camp (104B/1); in Geological Fieldwork 1986; British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1987-1, p. 81-92. Allen, D.G., Panteleyev, A., and Armstrong, A.T., 1976, Galore Creek; in Sutherland Brown, A., ed., Porphyry Deposits of the Canadian Cordillera: Canadian Institute of Mning and Metallurgy Special Volume 15, p. 402-414. Amato, J.M., and Wright, J.E., 1997, Potassic mafic magmatism in the Kigluaik gneiss dome, Northern <strong>Alaska</strong>; a geochemical study of arc magmatism in an extensional tectonic setting: Journal of Geophysical Research, v. 102, no. 4, p. 8065-8084. Amuzinsky, V.A., 1975, Low-sulfide gold-quartz assemblage of the Verkhoyansk meganticlinorium, in Ivensen, Yu.P., ed., Gold mineral assemblages and geochemistry of gold of the Verkhoyansk-Chukchi fold belt: Nauka, Moscow, p. 121-153 (in Russian). Anderson, H.E., and Davis, D.W., 1996, U-Pb geochronology of the Moyie sills, Purcell Supergroup, southeastern British
Columbia: Implicatons for the Middle Proterozoic geologic history of the Purcell (Belt) Basin: Canadian Journal of Earth Sciences, v. 32, p. 1180-1193. Anderson, R.G., 1983a, Geology of the Hotailuh Batholith and surrounding volcanic and sedimentary rocks, north-central British Columbia: Ottawa, Carleton University, Ph.D. dissertation, 669 p. Anderson, R.G., 1983b, Selwyn plutonic suite and its relationship to tungsten skarn mineralization, southeastern Yukon and District of Mackenzie: Current Research, Part B, Geological Survey of Canada, <strong>Paper</strong> 83-1B, p. 151-163. Anderson, R.G., and Reichenbach, I., 1991, U-Pb and K-Ar framework for Middle and Late Jurassic (172-158 Ma) and Tertiary (46-27 Ma) plutons on Queen Charlotte Islands, British Columbia, in Evolution and Hydrocarbon Potential of the Queen Charlotte Basin, British Columbia: Geological Survey of Canada <strong>Paper</strong> 90-10, p. 59-87. Andrew, A., Godwin, C.I., and Sinclair, A.J., 1983, Age and genesis of Cariboo gold mineralization determined by isotope methods (93H), in Geological Fieldwork 1982, British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1983-1, p. 305-313. Andrew, K.P.E., 1988, Geology and genesis of the Wolf precious metal epithermal prospect and the Capoose base and precious metal porphyry-style prospect, Capoose Lake area, central British Columbia: Vancouver, University of British Columbia, M.S. thesis, 334 p. Andrew, K.P.E., and Godwin, C.I., 1987, Capoose base and precious metal prospect, central British Columbia, in Geological Fieldwork 1986: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1987-1, p. 53-56. Andrew, K.P.E., Godwin, C.I., and Cann, R.M., 1986, Wolf epithermal precious metal vein prospect, central British Columbia, in Geological Fieldwork 1985: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1986-1, p. 317-320. Androsov, D.V. and Ratkin, V.V., 1990, Pre-folding massive zinc-sulfide ore in the Voznesenka greisen deposit (Primorye): Geologiya Rudnykh Mestorozhdeniy, no 5, p. 46-58 (in Russian). Anisimova, G.V., Gamyanin, G.N., Goryacheva, E.M., 1983, Native aluminum and chromium at the Sarylak deposit: Doklady Akademii Nauk SSSR, Moscow, v. 272, p. 657- 660 (in Russian). Anorov, P.N., and Mayuchaya, V.P., 1988, Features of porphyry mineralization occurrences in Magadan pluton— Magmatic and metamorphic complexes of the U.S.S.R. Northeast [abs.]: U.S.S.R. Academy of Sciences, North- Eastern Interdisciplinary Research Institute, Magadan, p. 99-100 (in Russian). References Cited 285 Apodaca, L.E., 1992, Fluid-inclusion study of the Rock Creek area, Nome mining district, Seward Peninsula, <strong>Alaska</strong>: 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. 3-12. Archer, A., Bell, R.T., and Thorpe, R.I., 1986, Age relationships from U-Th-Pb isotope studies of uranium mineralization in Wernecke breccias, Yukon Territory, in current Research, Part A: Geological Survey of Canada, <strong>Paper</strong> 86-1A, p. 385-391. Armstrong, R.L., 1988, Mesozoic and early Cenozoic magmatic evolution of the Canadian Cordillera, in Clark, S.P., Burchfiel, B.C., and Suppe, J., eds., Processes in continental lithospheric deformation: Geological Society of America Special <strong>Paper</strong> 218, p. 55-91. Armstrong, A.K., and MacKevett, E.M., Jr., 1982, Stratigraphy and diagenetic history of the lower part of the Triassic Chitistone Limestone, <strong>Alaska</strong>: U.S. Geological Survey <strong>Professional</strong> <strong>Paper</strong> 1212-A, 26 p. Armstrong, J.E., 1949, Fort St. James map-area, Cassiar and Coast districts: British Columbia, Geological Survey of Canada, Memoir 252, 210 p., scale 1 in. equals 6 mi. Armstrong, R.L., 1988, Mesozoic and early Cenozoic magmatic evolution of the Canadian Cordillera, in Clark, S.P., Jr., ed., Processes in Continental Lithosperic Deformation: Geological Association of America Special <strong>Paper</strong> 218, p. 55-91. Armstrong, R.L., Harakal, J.E., Forbes, R.B., Evans, B.W., and Thurston, S.P., 1986, Rb-Sr and K-Ar study of southern Brooks Range, in Evans, B.W., and Brown, E.H., eds., Blueschists and eclogites: Geological Society of America Memoir 164, p. 185-203. Armstrong, R.L., Harakal, J.E., and Hollister, V.F., 1976, Age determinations of late Cenozoic copper deposits of the North American Cordillera: Institute of Mining and Metallurgical Engineers Transactions, Section B, v. 85, p. 239-244. Armstrong, A.K., and MacKevett, E.M., Jr., 1982, Stratigraphy and diagenetic history of the lower part of the Triassic Chitistone Limestone, <strong>Alaska</strong>: U.S. Geological Survey <strong>Professional</strong> <strong>Paper</strong> 1212-A, 26 p. Armstrong, J.E., and and Roots, E.E., 1948, Geology and mineral deposits of Aiken Lake map-area, British Columbia: Geological Survey of Canada <strong>Paper</strong>, 46 p. Arth, J.G., 1994, Isotopic composition of the igneous rocks of <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. 781- 796. Arth, J.G., Barker, F., Stern, T.W., and Zmuda, C., 1986, The Coast batholith near Ketchikan, southeast <strong>Alaska</strong>; Geo-
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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
- Page 265 and 266: g/t Au or 368.2 Au gold. The deposi
- Page 267 and 268: wim Group and altered mafic dikes.
- Page 269 and 270: Mount Nansen porphyry Cu-Mo deposit
- Page 271 and 272: 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: margin or island-arc tectonic envir
- 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 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
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Valuy, G., and Rostovsky, F., 1988,
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Wolfe, W.J., 1995, Exploration and
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Appendix Table 1. Mineral deposit m
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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
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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
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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
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Table 3—Continued Metallogenic Be
- 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