USGS Professional Paper 1697 - Alaska Resources Library

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372 Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera Table 4—Continued Berezovka River Metallogenic Belt of Kuroko Massive Sulfi de and Sulfi de Vein Deposits (Late Devonian to Mississippian), Central Part of Russian Northeast (Belt BE) Berezovskoe Kuroko massive sulfi de and sulfi de vein Pb, Zn, Cu, Ag 66 º 43’N 157 º 21’E Mystic Metallogenic Belt of SEDEX Massive Bedded Barite and Southeast Missouri Pb-Zn Deposits (Devonian and Mississippian), West-Central Alaska (Belt MY) Gagaryah SEDEX massive bedded barite Cu, Ba 61 º 49’N 154 º 28’W Reef Ridge Southeast Missouri Pb-Zn Zn, Pb 63 º 29’N 154 º 20’W Northern Cordillera Metallogenic Belt of Southeast Missouri Zn-Pb Deposits (Late Proterozoic to Devonian) Central Yukon Territory (Belt NCO) Bear-Twit Southeast Missouri Pb-Zn Zn, Pb 64 º 03’N 129 º 25’W Gayna River Southeast Missouri Pb-Zn Zn, Pb 64 º 56’N 130 º 41’W Goz Creek Area (Barrier Reef) Southeast Missouri Pb-Zn Zn, Pb 64 º 23’N 132 º 31’W Rusty Springs (Termuende) Southeast Missouri Zn-Pb-Ag Ag, Zn, Cu 66 º 30’N 140 º 20’W Dempster Metallogenic Belt of SEDEX Ba, SEDEX Ni-Zn-PGE-Au, Kuroko Zn-Pb-Cu Massive Sulfi de Deposits (Devonian and Mississippian), Central Yukon Territory (Belt DE) Marg Kuroko Zn-Pb-Cu massive sulfi de Zn, Pb, Cu, Ag, Au 64 º 01’N 134 º 28’W Nick SEDEX Ni-Zn Ni, Zn, PGE 64 º 43’N 135 º 13’W Macmillan Pass Metallogenic Belt of SEDEX Zn-Pb-Ag-Ba Deposits (Devonian and Early Mississippian) Central Yukon Territory (Belt MP) Cathy (Bar, Walt, Hess) SEDEX Ba Ba, (Pb, Zn, Ag) 63 º 17’N 130 º 33’W Gravity (BA) SEDEX Ba Ba 63 º 44’N 128 º 52’W Jeff (Naomi, Baroid) SEDEX Ba Ba 63 º 37’N 129 º 40’W MacMillan Pass (Tom, Jason) SEDEX Pb-Zn Pb, Zn, Ag, Ba 63 º 10’N 130 º 12’W Moose (Spartan, Racicot) SEDEX Ba Ba 63 º 04’N 130 º 12’W Oro (Buc, Mar, Dar, Tang) SEDEX Ba Ba 62 º 37’N 129 º 46’W Tea (Brock) SEDEX Ba Ba 63 º 01’N 130 º 37’W Finlayson Lake Metallogenic Belt of SEDEX Zn-Pb-Ag-Cu-Au Deposits (Devonian and Mississippian) Southern Yukon Territory (Belt FL) Matt Berry SEDEX Pb-Zn Pb, Zn, Ag, Cu, Sb 61 º 29’N 129 º 24’W Liard Metallogenic Belt of Southeast Missouri Ba-F Deposits (Devonian), Southern Yukon Territory (Belt LI) Leguil Bedded Ba Ba 59 º 46’N 127 º 12’W Lower Liard Southeast Missouri Ba-F F, Ba 59 º 27’N 126 º 05’W Gataga Metallogenic Belt of SEDEX Zn-Pb-Ag-Ba Deposits (Devonian and Mississippian), Northern British Columbia (Belt GA) Akie SEDEX Zn-Pb Zn, Pb, Ag, Ba 57 º 13’N 124 º 29’W Cirque (Stronsay) (094F 008) SEDEX Pb-Zn Pb, Zn, Ag, Ba 57 º 31’N 125 º 09’W Driftpile Creek (Saint, Roen) (094K 066) SEDEX Pb-Zn Pb, Zn, Ba 58 º 05’N 125 º 54’W Robb Lake Metallogenic Belt of Southeast Missouri Zn-Pb-Ag Deposits (Devonian), Southern Northern Columbia (Belt RL) Robb Lake Southeast Missouri Pb-Zn Zn, Pb 57 º 22’N 123 º 52’W Southern Rocky Mountains Metallogenic Belt of Stratabound Barite-Magnesite-Gypsum Deposits (Early Paleozoic through Triassic), Southern British Columbia (Belt SRM) Brisco Area Ba vein and breccia Ba 50 º 50’N 116 º 20’W Forgetmenot Pass Stratbound gypsum Gypsum 53 º 45’N 119 º 53’W Kootenay River Gypsum Stratiform gypsum Gypsum 50 º 34’N 115 º 16’W Lussier River (United Gypsum) Stratiform gypsum Gypsum 50 º 03’N 115 º 31’W Marysville (082JNW 001) Stratiform magnesite Magnesite 49 º 36’N 115 º 58’W Mount Brussilof (Baymag) Stratabound Mg Magnesite 50 º 47’N 115 º 41’W Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Parson (082N 002) Barite vein and gypsum Ba 51 º 01’N 116 º 39’W Windermere Creek (Western Gypsum) Stratiform gypsum Gypsum 50 º 29’N 115 º 52’W
Table 4—Continued Appendix 373 Ingenika Metallogenic Belt of Southeast Missouri Zn-Pb-Ag Deposits (Devonian?), Southern British Columbia (Belt IN) Susie, Beverley and Regent Southeast Missouri Pb-Zn Pb, Zn, Ag, Ba 56 º 09’N 125 º 03’W Cathedral Metallogenic Belt of Southeast Missouri Zn-Pb-Ag Deposits (Devonian?), Southern British Columbia (Belt CA) Monarch (Kicking Horse) Southeast Missouri Zn-Pb-Ag Zn, Pb, Ag 51 º 25’N 116 º 26’W MISSISSIPPIAN (360 to 320 Ma) Northwestern Brooks Range Metallogenic Belt of SEDEX Zn-Pb, Kuroko Massive Sulfi de, Bedded Barite, and Vein Sulfi de Deposits (Mississippian and Pennsylvanian), Northwestern Alaska (Belt NBR) Drenchwater Sedimentary Zn-Pb and (or) kuroko massive sulfi de Zn, Pb, Ag 68 º 34’N 158 º 41’W Frost Cu-Zn-Pb-Ba vein Cu, Zn, Pb, barite 67 º 28’N 161 º 35’W Hannum Creek Metamorphosed SEDEX Zn-Pb? Pb, Zn, Ag 65 º 56’N 163 º 21’W Lik SEDEX Zn-Pb-barite Zn, Pb, Ag, Barite 68 º 12’N 163 º 07’W Nimiuktuk Bedded barite Barite 68 º 24’N 159 º 54’W Omar Kipushi Cu-Pb-Zn Cu, Pb, Zn, Ag, Co 67 º 30’N 161 º 50’W Red Dog Creek SEDEX Zn-Pb-barite Zn, Pb, Ag, Ba 68 º 04’N 162 º 50’W Story Creek Pb-Zn-Au-Ag vein Pb, Zn, Ag, Au 68 º 22’N 157 º 56’W Whoopee Creek Zn-Ag-Au vein Zn, Ag, Au 68 º 14’N 157 º 51’W PENNSYLVANIAN (320 to 286 Ma) Laoelin-Grodekovsk Metallogenic Belt of Porphyry Cu-Mo and Au-Ag Epithermal Vein Deposits (Permian) Southern Part of Russian Southeast (Belt LG) Baikal Porphyry Cu-Mo Cu, Mo 44 º 12’N 131 º 06’E Komissarovskoe (Vorob’eva plad) Au-Ag epithermal vein Au, Ag 44 º 34’N 131 º 27’E Aluchin Metallogenic Belt of Podiform Cr Deposits (Middle Paleozoic or older), Central Part of Russian Northeast (Belt AC) Teleneut Podiform Cr Cr, Ni 66 º 29’N 164 º 49’E Ust-Belaya Metallogenic Belt of Podiform Cr Deposits (Early Paleozoic), Northeastern Part of Russian Northeast (Belt UB) Ust-Belaya Podiform Cr Cr, PGE 65 º 27’N 173 º 04’E Alaska Range-Wrangell Mountains Metallogenic Belt of Granitic Magmatism Deposits (Pennsylvanian and Permian) Central and Eastern-Southern Alaska (Belt ARW) Chistochina District Porphyry Cu and polymetallic vein Cu, Pb, Ag, Au 63 º 05’N 144 º 47’W Rainbow Mountain Porphyry Cu Cu, Ag 63 º 20’N 145 º 41’W Rainy Creek District Cu-Ag skarn Cu, Ag, Au 63 º 20’N 146 º 02’W Slate Creek Porphyry Cu(?) Cu, Ag, Au 63 º 09’N 144 º 48’W Ketchikan Metallogenic Belt of Kuroko Massive Sulfi de Deposits (Pennsylvanian? or Permian?) Southeastern Alaska (Belt KK) Moth Bay Kuroko massive sulfi de Cu, Pb, Ag, Au 55 º 18’N 131 º 21’W LATE TRIASSIC (Carnian through Norian—230 to 208 Ma) Farewell Metallogenic Belt of Gabbroic Ni-Cu-PGE Deposits (Late Triassic), Western Alaska (Belt FW) Farewell District (Gargaryah, River Roberts, Straight Creek) Gabbroic Ni-Cu-PGE Ni, Cu, PGE 62 º 14’N 154 º 30’W Kodiak Island and Border Ranges Metallogenic Belt of Podiform Cr Deposits (Late Triassic, Early or Middle Jurassic) Southern Coastal Alaska (Belt KOD) Bernard Mountain, Dust Mountain Podiform Cr Cr, PGE 61 º 32’N 145 º 09’W Claim Point Podiform Cr Cr 59 º 12’N 151 º 49’W Halibut Bay Podiform Cr Cr 57 º 22’N 154 º 36’W Red Mountain Podiform Cr Cr 59 º 22’N 151 º 30’W Spirit Mountain Gabbroic Ni-Cu Ni, Cu, Co, Ag 61 º 19’N 144 º 13’W
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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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mentary rocks of the Cambrian to De
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(Preto and Schiarizza, 1985; Schiar
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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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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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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
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stocks and dikes, is associated wit
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etrograde minnesotaite (Fe talc), F
Page 295 and 296:
Specific Events for Early to Middle
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of fractured and faulted Permian-Tr
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sists of a mineralized fracture zon
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dolomite. Wall rock alteration incl
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elt of late Tertiary plutons that a
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plates that exhibit magnetic anomal
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stages (Petrenko, 1999): (1) In the
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mon. The deposit is of medium size
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Metallogenic-Tectonic Model for Lat
Page 313 and 314:
The origin of the Hg deposits of th
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margin or island-arc tectonic envir
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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 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
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 399 and 400: Table 4. Significant lode deposits,
Page 401 and 402: Table 4—Continued Appendix 369 De
Page 403: Table 4—Continued Tracy Metalloge
Page 407 and 408: Table 4—Continued Deposit Name Mi
Page 409 and 410: Table 4—Continued Mainits Metallo
Page 415 and 416: Table 4—Continued Whitehorse Meta
Page 421 and 422: Table 4—Continued Appendix 389 LA
Page 425 and 426: Table 4—Continued Surprise Lake M
Page 427 and 428: Table 4—Continued Sredinny Metall
Page 429: Table 4—Continued Deposit Name Mi
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