288 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera T.C., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining and Metallurgy, Special Volume 46, p. 623-629. Bliss, J.D., 1992, Grade and tonnage model of Chugach-type low-sulfide Au quartz veins, in Bliss, J.D., ed., 1992, Developments in mineral deposit modeling: U.S. Geological Survey Bulletin 2004, p. 41-46. Bliss, J.D., ed., 1992, Developments in mineral deposit modeling: U.S. Geological Survey Bulletin 2004, 168 p. Blodgett, R.B., 1998, Emsian (late Early Devonian) fossils indicate a Siberian origin for the Farewell terrane, in Clough, J.G., and Larson, F., eds., Short notes on <strong>Alaska</strong> geology 1997: <strong>Alaska</strong> Division of Geological and Geophysical Surveys <strong>Professional</strong> Report 118, p. 53-61. Blodgett, R.B., and Boucot, A.J., 1999, Late Early Devonian (Late Emsian) eospirifernid brachiopods from Shallabarger Pass, south-Central <strong>Alaska</strong>, and their biogeographic importance: Senckenbergiana Lethaea, v. 79, p. 209-221. Blodgett, R.B., and Brease, P.F., 1997, Emsian (Early Devonian) brachiopods from Shellabarger Pass, Talkeetna C-6 quadrangle, Denali National Park, <strong>Alaska</strong>, indicate Siberian origin for Farewell terrane [abs.]: Geological Society of America Program with Abstracts, v.29, p. 5. Blodgett, R.B., and Clough, J.G., 1985, The Nixon Fork terrane-part of an in-situ peninsular extension of the Paleozoic North American continent [abs.]: Geological Society of America Abstracts with Programs, v. 17, p. 342. Bloodgood, M.A., 1987, Geology of the Triassic black phyllite in the Eureka Peak area, central British Columbia (93A/7); in Gelogical Fieldwork 1986, British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> paper 1987-1, p. 135-142. Blum, J.D., 1985,. A petrologic and Rb-Sr isotopic study of intrusive rocks near Fairbanks, <strong>Alaska</strong>. Canadian Journal of Earth Sciences, v. 22, p. 1314-1321. Blusson, S.L., 1978, Regional geologic setting of lead- zinc deposits in Selwyn Basin, Yukon; Current research, Part A: Geological Survey of Canada, <strong>Paper</strong> 78-1A, p. 77-80. Bogdanov, N.A., Vishnevskaya, V.S., Kepezhinskas, P.K., Sukhov, A,N., and Fedorchuk, A.V., 1987, Geology of southern Koryak Highlands: Nauka, Moscow, 168 p. (in Russian). Bogovin, V.D., Kazanenko, G.G., Flerov, B.L., Ponamorev, V.G., Tychinsky, A.A., and Stepanov, E.P., 1979, The geologic setting and structure of deposits and the occurrences of ore bodies, in Kuznetsov, V.A., Yanshn, A.L., eds., Stratified lead-zinc deposits occurring in Vendian sequences in the southeastern Yalutiya: Nauka, Novosibirsk, p. 106-119 (in Russian). Bond, G.C., 1973, A late Paleozoic volcanic arc in the eastern <strong>Alaska</strong> Range, <strong>Alaska</strong>. Journal of Geology, v. 81, p. 557- 575. Bond, G.C., 1976, Geology of the Rainbow Mountain-Gulkana Glacier area, eastern <strong>Alaska</strong> Range, with emphasis on upper Paleozoic strata: <strong>Alaska</strong> Division of Geological and Geophysical Surveys Geologic Report 45, 47 p. Bond, J., 1983, Geology of the Tin Granite and associated skarn at Ear Mountain, Seward Peninsula, <strong>Alaska</strong>: Fairbanks, <strong>Alaska</strong>, University of <strong>Alaska</strong>, M.S. thesis, 89 p. Bouley, B.A., St. George, P., and Wetherbee, P.K., 1995, Geology and discovery at Pebble Copper, a copper-gold porphyry system in Southwest <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. 422-435. Bower, B., Payne, J., DeLong, C, and Rebagliati, C.M., 1995, The oxide-gold, supergene and hypogene zones at the Casino gold-copper-molybdenum deposit, west-central Yukon, in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America, Canadian Institute of Mining and Metallurgy Special Volume 46, p. 352-366. Box, S.E., 1985, Terrane analysis of the northern Bristol Bay region, southwestern <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. 32-37. Box, S.E., Moll-Stalcup, E.J., Frost, T.P., and Murphy, J.M., 1993, Preliminary geologic map of the Bethel and southern Russian Mission quadrangles, southwestern <strong>Alaska</strong>: U.S. Geological Survey Miscellaneous Field Studies Map MF- 2226-A, scale 1: 250,000, 20 p. Box, S.E., and Patton, W.W., Jr., 1989, Igneous history of the Koyukuk terrane, western <strong>Alaska</strong>: Constraints on the origin, evolution, and ultimate collision of an accreted island arc terrane: Journal of Geophysical Research, v. 94, p. 15,843- 15,867. Box, S.E., Moll-Stalcup, E.J., and Wooden, J.L., 1990, Kilbuck terrane—Oldest-known rocks in <strong>Alaska</strong>: Geology, v. 18, p. 1219-1222. Boyle, H.C., and Leitch, C.H.B., 1983, Geology of the Trout Lake molybdenum deposit, British Columbia: Canadian Institute of Mining and Metallurgy, Bulletin, 76, no. 849, p. 115-124. Bradford, J.A., and Godwin, C.I., 1988, Midway silver-leadzinc manto deposit, northern British Columbia, in Geological Fieldwork 1987: British Columbia Ministry of Energy, Mines, and Petroleum <strong>Resources</strong> <strong>Paper</strong> 1988-1, p. 353-360.
Bradley, D.C., Haeussler, P.J., and Kusky, T.M., 1993, Timing of early Tertiary ridge subduction in southern <strong>Alaska</strong>, in Dusel-Bacon, Cynthia, and Till, A.B., eds., Geologic Studies in <strong>Alaska</strong> by the U.S. Geological Survey, 1992: U.S. Geological Survey Bulletin 2068, p. 163-177. Brandon, M.T., Garver, J.I., Bullen, M.E., Sokovév, A.V., Ledneva, G.V., and Bogdanov, N.A., 1997, Eocene collision and obduction of the Olutorskiy island arc, Koryak Highlands of northern Kamchatka, Russian Far East [abs.]: Geological Society of America Abstracts with Program, v. 29, p. 6. Brandon, M.T., Garver, J.I., Bullen, M.E., Sokovév, A.V., Ledneva, G.V., and Bogdanov, N.A., 1998, Eocene collision and obduction of the Olutorskiy island arc, Koryak Highlands of northern Kamchatka, Russian Far East [abs.], in Abstracts of 6 th Zonenshain Conference on Plate Tectonics: Russian Academy of Sciences, Moscow, v. 29, p. 172. Brazhnik, A.V., and Kolyasnikov, Yu. A., 1989, Contemporary chemogenic precipitations in one of sulfide occurrences of the Koryak Highlands—Geology, geochemistry and minerals of the Far East: U.S.S.R. Academy of Sciences, North- Eastern Interdisciplinary Research Institute, Magadan, p. 50-63 (in Russian). Brazhnik, A.V., and Morozov, A.E., 1989, Peculiarities of metasomatic processes and ore matter balance in the Lalankytap porphyry molybdenum-copper deposit—Geochemistry and mineralogy of ore deposits of the U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, p. 142-155 (in Russian). Bremner, T., 1990, Brewery Creek, in Yukon Exploration 1990, Exploration and Geological Services Division: Indian and Northern Affairs Canada, p. 21-23. Bremmer, T.J., 1994, Geology and Metallogeny of southwest Yukon, in 1994 General Meeting, Abstracts and Proceedings of District: Canadian Institute of Mining, p. 38-44. Bremner, T., and Ouellette, D.,1991, Matt Berry, in Yukon Exploration 1990, Exploration and Geological Services Division: Indian and Northern Affairs Canada, p. 48-49. Brew, D.A., 1988, Latest Mesozoic and Cenozoic igneous rocks of southeastern <strong>Alaska</strong>—A synopsis. U.S. Geological Survey Open-File Report 88-405, 52 p. Brew, D.A., 1993, Regional geologic setting of mineral resources in southeastern <strong>Alaska</strong>, in Godwin, L.H., and Smith, B.D., eds., Economic mineral resources of the Annette Islands Reserve, <strong>Alaska</strong>: United States Department of the Interior, Bureau of Indian Affairs, Division of Energy and Mineral <strong>Resources</strong> Publication, p. 13-20. Brew, D.A., 1994, Latest Mesozoic and Cenozoic magmatism in southestern <strong>Alaska</strong>, in Plafker, George, and Berg, H.C., References Cited 289 eds., The Geology of <strong>Alaska</strong>: Boulder, Colorado, Geological Society of America, The Geology of North America, v. G-1, p. p. 621-656. Brew, D.A., and Ford, A.B., 1984, Tectonostratigraphic terrane analysis in the Coast plutonic-metamorphic complex, southeastern <strong>Alaska</strong>, in Reed, K. M., and Bartsch-Winkler, Susan, eds., The U.S. Geological Survey in <strong>Alaska</strong>—Accomplishments during 1982: U.S. Geological Survey Circular 939, p. 90-93. Brew, D.A., and Grybeck, Donald, 1984, Geology of the Tracy Arm-Fords Terror Wilderness Study Area and Vicinity, <strong>Alaska</strong>: U.S. Geological Survey Bulletin 1525-A, 52 p. Brew, D.A., Drew, L.J., Schmidt, J.M., Root, D.H. and Huber, D.F., 1991, Undiscovered locatable mineral resources of the Tongass National Forest and adjacent lands, southeastern <strong>Alaska</strong>: United States Department of the Interior, Geological Survey, Open-File Report 91-10, 369 p. Brew, D.A., Himmelberg, G.R., Loney, R.A., and Ford, A.B., 1992, Distribution and characteristics of metamorphic belts in the south-eastern <strong>Alaska</strong> part of the North American Cordillera: Journal of metamorphic geology, v. 10, p. 465-482. Brew, D.A., Himmelberg, G.R., Ford, A.B., and Loney, R.A., 1993, Magmatic and metamorphic belts and plutonic-metamorphic complexes of southeastern <strong>Alaska</strong> [abs.]. Geological Society of America Abstracts with Programs, v. 25, p. 13. Brew, D.A., Johnson, B.R., Grybeck, D., Griscom, A., and Barnes, D.F., 1978, Mineral resources study of the Glacier Bay National Monument wilderness study area, <strong>Alaska</strong>: United States Geological Survey Open-File Report 78-494, 678 p. Brew, D.A., and Morrell, R.P., 1983, Intrusive rocks and plutonic belts of southeastern <strong>Alaska</strong>, U.S.A.: Geological Society of America Memoir 159, p. 171-193. Bright, M.J., and Jonson D.C., 1976, Glacier Gulch (Yorke- Hardy), in Sutherland Brown, A., ed., Porphyry Deposits of the Canadian Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 15, p. 455-461 British Columbia Department of Mines, and Petroleum <strong>Resources</strong>, 1972, Geology, Exploration, and Mining in British Columbia, p. 272. British Columbia Department of Mines, and Petroleum <strong>Resources</strong>, 1991: Report 1991-7, 304 p. Brosge, W.P., and Reiser, H.N., 1968, Preliminary geologic and mineral resource maps (excluding petroleum), Arctic National Wildlife Range, <strong>Alaska</strong>: U.S. Geological Survey Open-File Report 76-539, 4 sheets, scale 1:500,000. Brostosvskaya, V.G., and Goncharov, V.I., Eremin, R.A., Savva, N.E., Sidorov, A.A., and Tolstikhin, Yu., V., 1974,
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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.
- 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 and 318: Columbia: Implicatons for the Middl
- Page 319: Bazard, D.R., Butler, R.F., Gehrels
- 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,
- Page 369 and 370: Wolfe, W.J., 1995, Exploration and
- Page 371 and 372:
Appendix Table 1. Mineral deposit m
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Table 2 Summary of correlations and
- Page 375 and 376:
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
- Page 415 and 416:
Table 4—Continued Whitehorse Meta
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Table 4—Continued Deposit Name Mi
- Page 419 and 420:
Table 4—Continued Appendix 387 De
- Page 421 and 422:
Table 4—Continued Appendix 389 LA
- Page 423 and 424:
Table 4—Continued Deposit Name Mi
- Page 425 and 426:
Table 4—Continued Surprise Lake M
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Table 4—Continued Sredinny Metall
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Table 4—Continued Deposit Name Mi