USGS Professional Paper 1697 - Alaska Resources Library

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370 Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera Table 4—Continued Kedon Metallogenic Belt of Au-Ag Epithermal Vein, Porphyry Mo, Fe Skarn, and Associated Deposits (Middle Paleozoic) Central Part of Russian Northeast (Belt KE) Grisha Au-Ag epithermal vein Au, Ag 63 º 48’N 159 º 28’E Kubaka Au-Ag epithermal vein Au, Ag 63 º 44’N 160 º 01’E Obyknovennoe Au-Ag epithermal vein Au, Ag 64 º 52’N 158 º 39’E Olcha Au-Ag epithermal vein Au, Ag 64 º 57’N 156 º 26’E Tumannaya Au-Ag epithermal vein Au, Ag 64 º 16’N 160 º 02’E Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Vechernee Porphyry Mo-Cu Mo, Cu 63 º 29’N 158 º 50’E Yolochka Au-Ag epithermal vein Au, Ag 63 º 33’N 159 º 38’E Zet Au-Ag epithermal vein Au, Ag 65 º 18’N 156 º 57’E Eastern Seward Peninsula (Kiwalik Mountain)Belt of Kuroko Massive Sulfi de Deposits (Middle Paleozoic) Northern Alaska (Belt ES) (No signifi cant deposits) Arctic Metallogenic Belt of Kuroko and Kipushi Massive Sulfi de Deposits (Devonian and Mississippian) Northern Alaska (Belt AT) Arctic Kuroko massive sulfi de Zn, Cu, Pb, Ag, Au 67 º 11’N 156 º 22’W BT, Jerri Creek Kuroko massive sulfi de Cu, Zn, Pb, Ag 67 º 08’N 155 º 52’W Michigan Creek Kuroko massive sulfi de As, Au, Ag, Cu, Zn, Pb 67 º 19’N 151 º 14’W Roosevelt Creek Kuroko massive sulfi de Cu, Zn, Pb, Ag, Au 67 º 10’N 152 º 30’W Ruby Creek, (Bornite) Kipushi Cu-Pb-Zn Cu, Co, Zn, Ag 67 º 04’N 156 º 59’W Smucker Kuroko massive sulfi de Cu, Zn, Pb, Ag 67 º 18’N 157 º 12’W Sun, (Picnic Creek) Kuroko massive sulfi de Cu, Zn, Pb, Ag, Au 67 º 04’N 155 º 01’W Brooks Range Metallogenic Belt of Granitic Magmatism Deposits (Devonian), Northern Alaska (Belt BR) Ann (Ernie Lake) Polymetallic vein (metamorphosed) Pb, Zn, Ag 67 º 25’N 152 º 50’W Bear Mountain Porphyry Mo Mo, W 68 º 23’N 142 º 11’W Esotuk Glacier Pb-Zn skarn and fl uorite vein Pb, Zn, Sn, Cu, W 69 º 18’N 145 º 15’W Galena Creek Polymetallic vein Cu, Zn, Pb, Ag 68 º 23’N 142 º 02’W Geroe Creek Porphyry Cu-Mo Cu, Mo 67 º 41’N 148 º 49’W Jim-Montana Cu-Zn skarn Cu, Zn, Ag, Pb 67 º 45’N 149 º 05’W Mount Igikpak and Arrigetch Polymetallic vein, Au quartz Cu, Pb, Zn, Ag, Au, 67 Peaks vein, Sn skarn, Cu-Pb-Zn skarn Sn, W, As º 26’N 154 º 07’W Porcupine Lake Polymetallic vein(?) Cu, Zn, Ag, F 68 º 48’N 146 º 27’W Romanzof Mountains Polymetallic vein, Pb-Zn and Pb, Cu, Zn, Mo, Sn, 69 possibly Sn skarn Ag, F º 18’N 143 º 50’W Sukakpak Mountain Sb-Au vein Au, Sb, Mo 67 º 36’N 149 º 50’W Victor, Venus, Evelyn Lee, and Porphyry Cu and Cu skarn Cu, Ag, Mo 67 º 38’N 149 º 20’W Ebo Alaska Range and Yukon-Tanana Upland Metallogenic Belt of Kuroko Massive Sulfi de Deposits (Devonian and Mississippian), Central and East-Central Alaska (Belt AKY) Anderson Mountain Kuroko massive sulfi de? Cu, Pb, Zn, Ag 63 º 48’N 147 º 57’W Delta District Kuroko massive sulfi de Pb, Zn, Cu, Ag, Au 63 º 14’N 144 º 10’W Liberty Bell Kuroko massive sulfi de(?) or polymetallic gold vein Au, Ag, Cu, Bi 64 º 37’N 148 º 51’W McGinnis Glacier Kuroko massive sulfi de Zn, Cu, Pb, Ag 63 º 36’N 146 º 14’W Miyaoka, Hayes Glacier Kuroko massive sulfi de Cu, Pb, Zn, Au, Ag 63 º 41’N 146 º 39’W Sheep Creek Kuroko massive sulfi de? Zn, Pb, Ag, Sn 63 º 54’N 148 º 17’W WTF, Red Mountain Kuroko massive sulfi de Cu, Pb, Zn, Ag, Au 63 º 45’N 147 º 22’W Dawson Metallogenic Belt of Volcanogenic Pb-Zn-Cu Massive Sulfi de, SEDEX Pb-Cu-Zn-Ba Deposits (Devonian and Mississippian), Central Yukon Territory (Belt DA) Lucky Joe Besshi massive sulfi de Cu, Zn, Pb 63 º 35’N 139 º 31’W Mickey SEDEX Zn-Pb Pyrite, Pb, Zn, Ba 64 º 19’N 140 º 29’W Lone Star Kuroko massive sulfi de Pb, Zn, Cu (Au, Ba) 63 º 53’N 139 º 13’W Frances Lake Metallogenic Belt of Volcanogenic Zn-Cu-Pb Massive Sulfi de Deposits (Devonian and Mississippian), Southern Yukon Territory (Belt FR) Kuda Ze Kayah (105G 117) Kuroko massive sulfi de Zn, Cu, Pb, Ag, Au 61 º 28’N 130 º 35’W Wolverine-Lynx (105G 072) Kuroko massive sulfi de Zn, Cu, Pb, Ag, Au 61 º 25’N 130 º 07’W
Table 4—Continued Tracy Metallogenic Belt of Kuroko Massive Sulfi de Deposits (Devonian and Mississippian) Southeastern Alaska (Belt TR) Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Alamo Kuroko massive sulfi de(?) Ag, Au, Cu, Zn 55 º 45’N 130 º 45’W Ecstall (103H 011) Kuroko Zn-Pb-Cu massive Zn, Cu, Au, Pb, 53 º 52’N 129 º 31’W sulfi de Ag, Fe Red River Kuroko massive sulfi de Cu, Mo 55 º 04’N 130 º 31’W Sumdum Kuroko massive sulfi de(?) Ag, Cu, Zn 57 º 47’N 133 º 28’W Sweetheart Ridge Kuroko massive sulfi de Ag, Au, Cu, Pb, Zn 57 º 55’N 133 º 37’W Mount Sicker Metallogenic Belt of Kuroko Volcanogenic Massive Sulfi de Zn-Cu-Pb-Au-Ag Deposits Mount Sicker (Lenora-Tyee (092b 001), Twin J, Lara (092B 129), Copper Canyon) Myra Falls (Lynx, Myra, Price, HW) (092F 330) (Devonian), Vancouver Island (Belt MS) Kuroko massive sulfi de Cu, Zn, Ag 48 º 52’N 123 º 47’W Kuroko massive sulfi de Zn, Cu, Ag, Au 49 º 34’N 125 º 36’W Kootenay-Shuswap Metallogenic Belt of Volcanogenic Zn-Pb-Cu-Ag-Au Massive Sulfi de Deposits (Devonian and Mississippian), Southern British Columbia (Belt KS) Chu Chua (082P 140) Cyprus massive sulfi de Cu, Zn, Au, Ag 51 º 23’N 120 º 04’W Goldstream (Pat) (082M 141) Besshi massive sulfi ce Cu, Zn, Ag 51 º 38’N 118 º 26’W Harper Creek (082M 009) kuroko massive sulfi de Cu, Ag, Au 51 º 31’N 119 º 49’W Homestake (Squaam Bay) (082M kuroko Zn-Pb-Cu massive Ag, Pb, Zn, Au, 51 025) sulfi de Cu, Ba º 07’N 119 º 50’W Rea (Hilton) kuroko Zn-Pb-Cu massive Ag, Pb, Zn, Au, Cu 51 º 09’N 119 º 49’W sulfi de Rexspar (Birch Island) Felsic plutonic U-REE U, F, Sr, REE, Th 51 º 34’N 119 º 54’W Khamna River Metallogenic Belt of Carbonatite-Related Nb, Ta, and REE Deposits (Devonian), Southern Part of Eastern Siberia (Belt KR) Gornoe Ozero Carbonatite-related REE REE, Ta, Nb 59 º 56’N 137 º 00’E Khamna Carbonatite-related REE REE, Nb 59 º 43’N 136 º 25’E Sette-Daban Range Metallogenic Belt of Southeast Missouri Pb-Zn, Sediment-Hosted Cu, and Basaltic Cu Deposits (Late Proterozoic), Southern Part of Eastern Siberia (Belt SD) Dzhalkan Basaltic Cu Cu 63 º 38’N 136 º 38’E Kurpandja Sediment-hosted Cu Cu 63 º 31’N 137 º 01’E Lugun Southeast Missouri Pb-Zn Pb, Zn 59 º 08’N 136 º 39’E Sakyryr Southeast Missouri Pb-Zn Zn, CaF2 62 º 43’N 138 º Sardana Southeast Missouri Pb-Zn Pb, Zn 22’E 60 º 06’N 136 º 45’E Segenyakh Southeast Missouri Pb-Zn Pb, Zn, CaF2 63 º 10’N 137 º Urui Southeast Missouri Pb-Zn Pb, Zn 51’E 59 º 52’N 136 º 47’E Selennyakh River Metallogenic Belt of Southeast Missouri Pb-Zn, Stratabound Hg and Au, and Pb-Zn Vein Deposits (Devonian to Permian), Northwestern Part of Russian Northeast (Belt SEL) Chistoe Pb-Zn vein Pb, Zn 68 º 12’N 141 º 26’E Gal-Khaya Carbonate-hosted Hg Hg 68 º 53’N 140 º 18’ Khatynnakh-Sala Au quartz vein Au 68 º 18’N 141 º 24’E Kondakovskoe Southeast Missouri Pb-Zn Pb, Zn 69 º 19’N 149 º 49’E Tommot River Metallogenic Belt of Carbonatite-Related Nb, Ta, and REE Deposits (Devonian to Mississippian) Northwestern Part of Russian Northeast (Belt TO) Tommot Carbonatite-related REE (Ta, REE, Ta, Nb 68 º 24’N 141 º 14’E Nb) Appendix 371 Urultun and Sudar Rivers Metallogenic Belt of Southeast Missouri Pb-Zn, Carbonate-Hosted Hg, Basaltic Cu and Volcanogenic Mn Deposits (Devonian and Carboniferous), West-Central Part of Russian Northeast (Belt URS) Batko Basaltic Cu Cu 63 º 25’N 149 º 42’E Lyglykhtakh Sedimentary Mn Mn 62 º 59’N 151 º 20’E Prizovoe Bedded barite Ba 63 º 29’N 149 º 34’E Prolivnoe Southeast Missouri Pb-Zn Pb, Zn 63 º 30’N 149 º 18’E Uochat Carbonate-hosted Hg Hg 63 º 45’N 148 º 45’E Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Urultun Southeast Missouri Pb-Zn Pb, Zn 63 º 40’N 148 º 42’E Yarkhodon Metallogenic Belt of Southeast Missouri Pb-Zn Deposits (Late Devonian to Mississippian) Central Part of Russian Northeast (Belt YR) Slezovka Southeast Missouri Pb-Zn Pb, Zn 66 º 51’N 153 º 54’E Gornoe Southeast Missouri Pb-Zn Pb, Zn 66 º 36’N 154 º 19’E
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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
Page 289 and 290:
during back-arc extension or transt
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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 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: Table 4—Continued Appendix 369 De
Page 405 and 406: Table 4—Continued Appendix 373 In
Page 407 and 408: Table 4—Continued Deposit Name Mi
Page 409 and 410: Table 4—Continued Mainits Metallo
Page 413 and 414: Table 4—Continued Appendix 381 De
Page 415 and 416: Table 4—Continued Whitehorse Meta
Page 419 and 420: Table 4—Continued Appendix 387 De
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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