286 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera chronology and geochemistry [abs.]: Geological Society of America Abstracts with Programs, v. 18, p. 529. Ash, C.H., Macdonald, R.W.J., and Friedman, R.M., 1997, Stratigraphy of the Tatogga Lake area, northwestern British Ciolumbia (104H/12, 13; 104G19, 16), in Geological Fieldwork, 1996: British Columbia Ministry of Energy and Mines, p. 283-290. Ashleman, J.C., Taylor, C.D., and Smith, P.R., 1997, Porphyry Mo deposits of <strong>Alaska</strong>, with emphasis on the geology of the Quartz Hill deposit, southeastern <strong>Alaska</strong>, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of <strong>Alaska</strong>: Economic Geology Monograph 9, p. 334-354. Asher, R.R., 1969, Geologic and geochemical study, Solomon C-5 quadrangle, Seward Peninsula, <strong>Alaska</strong>: <strong>Alaska</strong> Division of Mines and Geology Report 33, 64 p. Ashworth, Kate, 1983, Genesis of gold deposits of Little Squaw Mine, Chandalar District, <strong>Alaska</strong>: Bellingham, Washington, Western Washington University, M.S. thesis, 64 p. Atkinson, D., 1995, The Glacier Gulch (Hudson Bay Mountain or Yorke Hardy) porphyry molybdenum-tungsten deposit, west-central 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. 704-707. Atkinson, D., and Baker, D.J.,1986, Recent developments in the geologic understanding of Mactung, in Morin, J.A., ed., Mineral Deposits of Northern Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 37, p. 234-244. Babkin, P.V., 1975, Mercury provinces of the U.S.S.R. Northeast: Nauka, Novosibirsk, 168 p. (in Russian). Babkin, P.V., Drabkin, I.E., and Kim, E.P., 1967, Volcanichosted mercury mineralization of the Magadan region: Ore Capacity of Volcanogenic Formations in the Northeast and Far East: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, p. 133-140 (in Russian). Bakharev, A.G., Gamyanin, G.N., Goryachev, and N.A., Polovinkin, V.L., 1988, Magmatic complexes and mineral assemblages of the Ulakhan-Tas Range, the northeast Yakutia: U.S.S.R. Academy of Sciences, Siberian Branch, Institute of Geology, Yakutsk, 199 p. (in Russian). Bakke, A.A., 1995, The Fort Knox “porphyry” gold deposit— Structurally-controlled stockwork and shear quartz vein, sulfide-poor mineralization hosted by a Late Cretaceous pluton, 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. 795-802. Baranov, B.V., Seliverstov, N.I., Muravov, A.V., and Muzuzov, E.L., 1991, The Komandorsky Basin as a product of spreading behind a transform plate boundary: Tectonophysics, v. 199, p. 237-269. Barker, Fred, 1994, Some accreted volcanic rocks of <strong>Alaska</strong> and their elemental abundances, 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. 555-588. Barker, Fred, and Stern, T.W., 1986, An arc-root complex of Wrangellia, eastern <strong>Alaska</strong> Range [abs.]: Geological Society of America Abstracts with Programs, v. 18, no. 6, p. 534. Barker, Fred, Sutherland-Brown, A., Budahn, J.R., and Plafker, G., 1989, Back-arc with frontal-arc component origin of Triassic Karmutsen basalt, British Columbia, Canada: Chemical Geology, v. 75, p. 81-102. Barker, J.C., 1987, Distribution of platinum group elements in an ultramafic complex near Rainbow Mountain—<strong>Alaska</strong>: Process Mineralogy VII: Applications to Exploration, Warren, Pennsylvlania, p. 197-200. Barker, J.C., and Swainbank, R.C., 1986, A tungsten-rich porphyry molybdenum occurrence at Bear Mountain, northeast <strong>Alaska</strong>: Economic Geology, v. 81, p. 1753-1759. Bakulin, Y.I., Burak, V.A., Galuchanun, Y.H., Lowshak, N.P., and Romanovksy, N.P., 1999, Mineral resources of Khabarovsk, Amur, and Primorye Regions, Far East Economic Zone, Russian Federation: Russian Ministry of Natural <strong>Resources</strong>, Khabarovsk Office, Special Annual Publication, 213 p. (in Russian). Barr, D.A., 1980, Gold in the Canadian Cordillera: Canadian Institute of Mining and Metallurgy Bulletin, v. 73, p. 59-76. Barrett, T.J., and Sherlock, R.L., 1996, Volcanic stratigraphy, lithogeochemistry, and seafloor setting of the H-W massive sulphide deposit, Myra Falls, Vancouver Island, British Columbia: Exploration and Mining Geology, v. 5, p. 421- 458. Barrie, C.T., 1993, Petrochemistry of shoshonitic rocks associated with porphyry copper-gold deposits of central Quesnellia, British Columbia: Journal of Geochemical Exploration, v. 48, p. 225-258. Bateman, A.M., and McLaughlin, D.H., 1920, Geology of the ore deposits of Kennecott, <strong>Alaska</strong>: Economic Geology, v. 15, p. 1-80. Bazard, D.R., Butler, R.F., Gehrels, G.E., 1993, Paleomagnetic and detrital zircon analysis of the Lower Devonian Karheen Formation, Alexander Terrane, southeastern <strong>Alaska</strong> [abs.]: Eos, Transactions, American Geophysical Union, v. 74, p. 213.
Bazard, D.R., Butler, R.F., Gehrels, G.E., and Soja, C.M., 1994, New constraints for Late Silurian-Devonian paleogeography of the Alexander terrane, southeastern <strong>Alaska</strong> [abs.]: Geological Society of America Abstracts with Program, v. 26, p. 384. Bazhanov, V.A., 1988, Major geological and metallogenic features of the Khanka massif, in Kokorin, A.M., ed., Metallogeny of major tin-bearing districts of the southern Russian Far East: Far East Geological Institute, Vladivostok, p. 114- 133 (in Russian). Beard, J.S., and Barker, Fred, 1989, Petrology and tectonic significance of gabbros, tonalites, shoshonite, and anorthosites in a late Paleozoic arc-root complex in the Wrangellia terrane, southern <strong>Alaska</strong>: Journal of Geology, v. 97, p. 667-683. Beaudoin, G., Roddick, J.C., and Sangster, D.F., 1992, Eocene age for Ag-Pb-Zn-Au vein and replacement deposits of the Kokanee Range, southeastern British Columbia: Canadian Journal of Earth Sciences, v. 29, p. 3-14. Bekhtold, A.F., and Semenov, D.F., 1990, Metabasites and ultramafic rocks of the Susunai Ridge (Sakhalin Island): Tikhookeanskaya Geologiya, no. 1, p. 121-125 (in Russian). Belasky, P., and Runnegar, B., 1994, Permian longitudes of Wrangellia, Stikinia, and eastern Klamath terranes based on coral biogeography: Geology, v. 22, p. 1095-1098. Bell, R.T., 1968, Proterozoic stratigraphy of northeastern British Columbia: Geological Survey of Canada <strong>Paper</strong> 67-68, 75 p. Bell, R.T., 1991, Uranium and thorium, 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. 782-787. Bely, V.F., 1977, Stratigraphy and structures of the Okhotsk- Chukotka volcanogenic belt: Nauka, Moscow, 171 p (in Russian). Bely, V.F., 1978, Formations and tectonics of the Okhotsk- Chukotka volcanogenic belt: Nauka, Moscow, 213 p (in Russian). Belytsky, B.V., and Krymsky, R.S., 1999, Age and genetic relationship of rare-metal ore-bearing granites of Voznesenka ore field, Primorye—Rb-Sr and Sm-Nd isotopic data, in C.J. Stanley and others, eds., Mineral Deposits: Processes to Processing: A.A. Balkema/Rotterdam/Brookfield, v. 1, p. 313-316. Benevolsky, B.I., Migachev, I.F., and Schepotiev , Yu.M., 1992, The state and potential of gold resources of the Commonwealth of Independent States under the new market conditions: Sovietskaya Geologiya, no. 3, p. 4-11 (in Russian). Berg, H.C., 1984, Regional geologic summary, metallogenesis, and mineral resources of southeastern <strong>Alaska</strong>: U.S. References Cited 287 Geological Survey Open-File Report 84-572, 298 p., scale 1:600,000. Berg, H.C., and Cobb, E.H., 1967, Metalliferous lode deposits of <strong>Alaska</strong>: United States Geological Survey Bulletin 1246, 254 p. Berg, H.C., and Grybeck, Donald, 1980, Upper Triassic volcanogenic Zn-Pb-Ag (Cu-Au)-barite mineral deposits near Petersburg, <strong>Alaska</strong>: U.S. Geological Survey Open-File Report 80-527, 9 p. Berg, H.C., Decker, J.E., and Abramson, B.S., 1981, Metallic mineral deposits of southeastern <strong>Alaska</strong>: U.S. Geological Survey Open-File Report 81-122, 136 p., 1 sheet, scale 1:1,000,000. Berg, H.C., Elliott, R.L., and Koch, R.D., 1978, Map and tables describing areas of metalliferous mineral resource potential in the Ketchikan and Prince Rupert quadrangles, <strong>Alaska</strong>: U.S. Geological Survey Open-File Report 78-73M, 48 p., 1 sheet, scale 1:250,000. Berg, H.C., Jones, D.L., and Richter, D.H., 1972, Gravina- Nutzotin belt—Tectonic significance of an upper Mesozoic sedimentary and volcanic sequence in southern and southeastern <strong>Alaska</strong>: U.S. Geological Survey <strong>Professional</strong> <strong>Paper</strong> 800-D, p. D1-D24. Berger, V.I., 1978, Antimony deposits (regularities of distribution and criteria for prediction): Nedra, Leningrad, 296 p. (in Russian). Berger, V.I., 1993, Descriptive model of gold-antimony deposits: U.S. Geological Survey Open-File Report 93-194, 24 p. Berman, Yu. S., 1969, Gold-argentite assemblage as one of features of gold-silver deposits: Transactions of Central Research Geological-Exploratory Institute, v. 86, part 1, p. 39-43 (in Russian). Berman, Yu. S., and Trenina, T.I., 1968, Gold in gold-silver occurrences and related placers in Chukotka: Transactions of Central Research Geological-Exploratory Institute, 79, p. 142-152 (in Russian). Beus, V.A., and Miledin, A.K., 1990, New age data for the metamorphic complex of the Prikolymian Uplift: Reports of the U.S.S.R. Academy of Sciences, v. 311, no. 4, p.925-928 (in Russian). Binda, P.L., Koopman, H.T., and Koopman, E.R., 1989, A stratiform copper occurrence in the Helikian Siyeh Formation of Alberta, 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. 269-286. Bishop, S.T., Heah, T.S., Stanley, C.R., and Lang, J.R., 1995, Alkalic intrusion hosted copper-gold mineralization at the Lorraine deposit, north-central British Columbia, in Schroeter,
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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
- 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 and 316: margin or island-arc tectonic envir
- Page 317: Columbia: Implicatons for the Middl
- 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
- Page 367 and 368: 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
- 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,
- Page 401 and 402:
Table 4—Continued Appendix 369 De
- Page 403 and 404:
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
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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