USGS Professional Paper 1697 - Alaska Resources Library

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386 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Table 4—Continued Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Kandychan Sn polymetallic vein Sn, Ag 60 º 36’N 150 º 20’E Kharan Sn polymetallic vein Sn 61 º 56’N 146 º 03’E Khenikandja Sn silicate-sulfi de and Sn polymetallic vein Sn 61 º 49’N 146 º 31’E Kheta Sn polymetallic vein Sn, Zn, Pb, Cu, Bi, Ag 61 º 06’N 151 º 47’E Khuren Sn polymetallic vein Sn 60 º 54’N 147 º 10’E Kuranakh-Sala Sn silicate-sulfi de vein Sn 63 º 03’N 144 º 19’E Kyurbelykh Sn silicate-sulfi de vein and Sn Sn 62 º 46’N 145 º 29’E polymetallic vein Netchen-Khaya Granitoid-related Au Au, Mo, Bi 61 º 42’N 151 º 32’E Ossolonyn Sn greisen Sn 61 º 43’N 153 º 19’E Porozhistoe Sn polymetallic vein Sn 61 º 36’N 146 º 28’E Shkolnoe Granitoid-related Au Au 61 º 28’N 148 º 48’E Suvorov Rhyolite-hosted Sn Sn 61 º 00’N 152 º 09’E Svetloe Sn polymetallic vein Sn 60 º 46’N 150 º 16’E Tankist Porphyry Mo Mo 61 º 21’N 147 º 56’E Tektonicheskoe Pb-Zn-Ag vein Pb, Zn, Ag, Sn 62 º 26’N 145 º 15’E Tigrets-Industriya Sn polymetallic vein Sn, Ag, Pb, Zn 62 º 16’N 146 º 31’E Verkhne-Seimkan Co-Bi-As vein Co, Bi 60 º 31’N 149 º 60’E Zerkalnoe Au-Ag epithermal vein Au, Ag, Bi, Te 60 º 58’N 151 º 10’E Vostochno-Verkhoyansk Zone (Eastern Asia-Arctic metallogenic belt) of Ag Polymetallic Vein Deposits (Late Cretaceous and early Tertiary), West-Central Part of Russian Northeast (Belt EAVV) Altaiskoe Ag polymetallic vein Pb, Zn, Ag 63 º 01’N 140 º 43’E Bezymyannoe Ag polymetallic vein Ag, Pb 65 º 39’N 130 º 36’E Imtachan Sn polymetallic vein Pb, Zn, Sn 62 º 57’N 139 º 44’E Kuolanda Ag polymetallic vein Pb, Zn, Ag 67 º 11’N 127 º 45’E Mangazeika Ag polymetallic vein Pb, Ag 65 º 46’N 130 º 35’E Prognoz Ag polymetallic vein Ag, Pb 65 º 41’N 133 º 29’E Verkhnee Menkeche Ag polymetallic vein Pb, Zn, Ag 62 º 56’N 139 º 27’E Adycha-Taryn Zone (Eastern Asia-Arctic Metallogenic Belt) of Clastic Sediment-Hosted Sb-Au, Au-Ag Epithermal Vein, and Ag-Sb Polymetallic Vein Deposits (Cretaceous and early Tertiary), Western Part of Russian Northeast (Belt EAAT) Ak-Altyn Au-Ag epithermal vein Au 67 º 02’N 133 º 60’E Billyakh Au-Sb polymetallic vein Sb, Au 67 º 35’N 134 º 06’E Maltan Sb-Au vein Au, Sb 64 º 03’N 143 º 19’E Sarylakh Sb-Au vein Au, Sb 64 º 17’N 142 º 46’E Sentachan Sb-Au vein or clastic sedimenthosted Sb-Au Sb 66 º 29’N 137 º 03’E Uzlovoe Sb-Au vein or clastic sediment- Au, Sb 66 º 06’N 137 º 48’E hosted Sb-Au Omsukchan Zone (Eastern Asia-Arctic Metallogenic Belt) of Sn Polymetallic Vein, Sn Silicate-Sulfi de, Porphyry Sn, Ag Epithermal Vein, Porphyry Mo-Cu, and Associated Deposits (Late Cretaceous) Southeastern Part of Russian Northeast (Belt EAOM) Arylakh Au-Ag epithermal vein Ag, Au 63 º 08’N 154 º 58’E Dukat Au-Ag epithermal vein Ag, Au 62 º 36’N 155 º 11’E Egorlyk Sn silicate-sulfi de vein Sn 63 º 27’N 154 º 55’E Elombal, Yakor Sb-Au vein? Au, As, Sb 67 º 45’N 165 º 27’E Galimoe Sn silicate-sulfi de vein Sn, Ag 62 º 21’N 155 º 49’E Ircha Porphyry Sn Sn, Ag 61 º 51’N 155 º 39’E Khataren-Industrial Sn silicate-sulfi de vein Sn 62 º 33’N 155 º 34’E Maly Ken Sn polymetallic vein Sn, Ag 62 º 44’N 154 º 60’E Mechta Ag-Pb-Zn vein , Polymetallic Ag, Pb, Zn 62 º 48’N 155 º 05’E vein(?) Nevskoe Porphyry Sn Sn, W, Se 62 º 16’N 155 º 26’E Novy Djagyn Porphyry Sn Sn 62 º 48’N 155 º 25’E Okhotnichie Sn silicate-sulfi de vein Sn 62 º 04’N 155 º 14’E Podgornoe Au-Co-As vein Au, Co, Bi, Te, (As) 62 º 37’N 155 º 48’E
Table 4—Continued Appendix 387 Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Rogovik Au-Ag epithermal vein Ag, Au 64 º 18’N 153 º 58’E Tidit Ag-Pb-Zn vein, Polymetallic vein(?) Ag, Pb, Zn 62 º 51’N 155 º 11’E Trood Sn polymetallic vein Sn, Pb Zn, Ag 62 º 04’N 155 º 42’E Chokurdak Metallogenic Belt of Granitoid-Related Sn Greisen, Sn-Polymetallic Vein, Sn Greisen, and Au-Ag Epithermal Vein Deposits (Early and mid-Cretaceous), Northern Part of Russian Northeast (Belt CD) Chokurdakh Sn silicate tourmaline, Sn silicate-sulfi de vein Sn 72 º 14’N 140 º 18’E Churpunnya Sn silicate-sulfi de vein Sn 71 º 06’N 141 º 43’E Deputatskoe Sn polymetallic vein(?) Sn 69 º 15’N 139 º 58’E Djaktardakh Sn polymetallic vein Sn 69 º 10’N 141 º 20’E Khomustak Sn greisen Sn 70 º 05’N 152 º 28’E Odinokoe Sn greisen Sn 69 º 42’N 142 º 01’E Pavel-Chokhchurskoe Sn polymetallic vein and greisen Sn 70 º 10’N 140 º 48’E Primorskoe Sn polymetallic vein Sn 69 º 56’N 153 º 22’E Sigilyakh Sn silicate-sulfi de vein Sn 69 º 54’N 136 º 47’E Ukachilkan Sn polymetallic vein Sn 69 º 55’N 139 º 19’E Yuzhnoe Polymetallic vein Pb, Zn 69 º 31’N 150 º 42’E Chaun Zone (Eastern Asia-Arctic Metallogenic Belt) of Granitic-Magmatism-Related Deposits (Late Cretaceous) Northeastern Part of Russian Northeast (Belt EACN) Barin Ag polymetallic vein and replacement Ag, Zn 66 º 22’N 172 º 04’W Chechekuyum Pb-Zn skarn Pb, Zn, Cu, Ni 64 º 36’N 172 º 45’W Dioritovoe Sn polymetallic vein Sn 65 º 40’N 174 º 06’W Ekug Porphyry Sn or Sn greisen Sn, W 67 º 34’N 178 º 04’W Elmaun Sn silicate-sulfi de vein Sn 66 º 19’N 179 º 46’W Enpylkhkan Pb-Zn skarn Pb, Zn, Cu, Ag 65 º 20’N 174 º 16’W Erulen Sn silicate-sulfi de vein Sn 66 º 09’N 173 º 17’W Eruttin Sn silicate-sulfi de vein Sn 66 º 24’N 178 º 55’W Granatnoe Porphyry Mo Mo 67 º 12’N 179 º 09’W Ichatkin Sn silicate-sulfi de vein Sn 69 º 41’N 163 º 11’E Kekur Sn silicate-sulfi de vein Sn 69 º 49’N 171 º 52’E Kuekvun Granitoid-related Au Au, Bi, Te, Sn, W 68 º 46’N 178 º 53’E Kukenei Sn polymetallic vein Sn, Ag 69 º 08’N 174 º 05’E Lunnoe Sn silicate-sulfi de vein Sn, W 68 º 49’N 174 º 49’E Melyul Pb-Zn-(Cu)-Ag skarn Pb, Zn, Ag, (Cu) 66 º 16’N 172 º 04’W Mramornoe Sn polymetallic vein Sn, Ag 68 º 06’N 176 º 30’E Mymlerennet Sn silicate-sulfi de vein Sn 67 º 47’N 179 º 46’E Pepenveem Au-Ag epithermal vein Au, Ag 65 º 52’N 175 º 37’W Pyrkakai Porphyry Sn Sn, W 69 º 33’N 171 º 57’E Reechen Fe-Pb-Zn-Sn skarn Fe, Pb, Zn, Sn 64 º 57’N 172 º 29’W Serdtse-Kamen Pb-Zn skarn Pb, Zn, Cu, Sn, Ag 66 º 50’N 171 º 44’W Shurykan Porphyry Cu-Mo Mo, Cu 68 º 44’N 174 º 23’E Telekai Sn silicate-sulfi de vein and Sn greisen Sn 67 º 59’N 178 º 05’E Tumannoe Disseminated Au-sulfi de Au, As, Sb 67 º 40’N 178 º 06’W Valkumei Sn silicate-sulfi de vein Sn 69 º 39’N 170 º 12’E Vodorazdelnoye Sn silicate-sulfi de vein Sn 67 º 55’N 178 º 51’E Yassnoe Clastic sediment-hosted Hg or hot-spring Hg? Hg 68 º 23’N 167 º 48’E Chukotka Metallogenic Belt of Au Quartz Vein and Sn and Sn-W Polymetallic Vein Deposits (Early Cretaceous) Northern Part of Russian Northeast (Belt CH) Chaantal Sn quartz vein and Sn greisen Sn, W 67 º 52’N 179 º 25’W Dvoinoi Au quartz vein Au 69 º 33’N 176 º 02’E Iultin Sn quartz vein Sn, W 67°51’N 178°44’W Karalveem Au quartz vein Au 68 º 11’N 166 º 09’E Lenotap Au quartz vein Au 67 º 47’N 178 º 47’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
Page 273 and 274:
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
Page 297 and 298:
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
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 and 402: Table 4—Continued Appendix 369 De
Page 403 and 404: Table 4—Continued Tracy Metalloge
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 417: Table 4—Continued Deposit Name Mi
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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