USGS Professional Paper 1697 - Alaska Resources Library

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384 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. Iskra Sn polymetallic vein Sn, 44 º 13’N 134 º 32’E Khrustalnoe Sn silicate-sulfi de vein Sn 44 º 28’N 134 º 59’E Lazurnoe Porphyry Cu-Mo Cu, Mo 44 º 06’N 134 º 24’E Malinovskoe Porphyry Cu Cu 45 º 08’N 135 º 02’E Nizhnee Sn polymetallic vein Sn, Pb, Zn 43 º 37’N 134 º 15’E Smirnovskoe Polymetallic vein Pb, Zn, Sn 44 º 38’N 135 º 20’E Tigrinoe Sn-W greisen Sn, W, Ta, Nb, In 46 º 05’N 135 º 45’E Verkhnezolotoe Porphyry Cu Cu, Sn 46 º 32’N 136 º 26’E Vysokogorskoe Sn silicate-sulfi de vein Sn 44 º 21’N 135 º 10’E Yantarnoe Porphyry Sn Sn 46 º 20’N 136 º 34’E Yuzhnoe Polymetallic vein Pb, Zn, Ag 44 º 45’N 135 º 21’E Zabytoe W-Sn greisen W, Sn, Bi 45 º 39’N 135 º 25’E Zarechnoe Porphyry Cu Cu 44 º 39’N 134 º 39’E Zimnee Sn polymetallic vein Sn, Pb, Zn 45 º 46’N 135 º 58’E Zvezdnoe Porphyry Sn Sn 46 º 10’N 136 º 30’E Lower Amur Metallogenic Belt of Au-Ag Epithermal Vein, Porphyry Cu, and Sn Greisen Deposits (mid-Cretaceous to early Tertiary), Northern Part of Russian Southeast (Belt LA) Belaya Gora Au-Ag epithermal Vein Au, Ag 53 º 23’N 140 º 14’E Bichinskoe Sn greisen W, Sn 52 º 32’N 139 º 32’E Bukhtyanskoe Au-Ag epithermal vein Au, Ag 53 º 03’N 140 º 29’E Mnogovershinnoe Au-Ag epithermal vein Au, Ag 53 º 53’N 139 º 48’E Tyrskoe Porphyry Cu Cu 52 º 57’N 140 º 27’E Aniva-Nabil Metallogenic Belt of Volcanogenic Mn and Fe and Cyprus Massive Sulfi de Deposits (Late Cretaceous), Eastern Part of Russian Southeast (Belt LA) Bereznyakovskoe Volcanogenic Mn Mn 47 º 04’N 142 º 56’E Lyukamskoe Volcanogenic Mn Mn 49 º 58’N 143 º 35’E Novikovskoe Cyprus massive sulfi de(?) Cu, Zn, Pb 46 º 18’N 143 º 26’E Rys’e Cyprus massive sulfi de Cu, Pb, Zn 49 º 31’N 144 º 01’E Koryak Highlands Metallogenic Belt of Zoned Mafi c-Ultramafi c PGE Deposits (Upper Cretaceous) East-Central Part of Russian Northeast (Belt KH) Karagin group Gabbroic Cu Cu, Zn, Au, Pt, Ni, 58 º 52’N 164 º 02’E Snezhnoe Zoned mafi c-ultramafi c Cr-PGE Cr, PGE 61 º 37’N 171 º 39’E Galmeonsky-Seinavsky <strong>Alaska</strong>n PGE PGE, Cr 61 º 34’N 166 º 05’E Vatyn Metallogenic Belt of Volcanogenic Mn and Fe Deposits (Early Cretaceous), Southeastern Part of Russian Northeast (Belt VT) Itchayvayam Volcanogenic Mn Mn 61 º 24’N 172 º 20’E Dogdo-Erikit Zone (Eastern Asia-Arctic Metallogenic Belt) of Au-Ag Epithermal Vein, Sn-polymetallic vein (Southern Bolivian type?), and Volcanic-Hosted Hg (Plamennoe type) Deposits (Late Cretaceous and early Tertiary) West-Central Part of Russian Northeast (Belt EADE) Dogdo Volcanic-hosted Hg Hg 67 º 21’N 139 º 27’E Kysylga Au-Ag epithermal vein Au, Ag 67 º 33’N 137 º 55’E Shirokoe Au-Ag epithermal vein Au, Ag 65 º 36’N 144 º 33’E Solkuchan (Khatys) Sn polymetallic vein Ag, Sn 65 º 15’N 143 º 51’E Tikhon Au-Ag epithermal vein Ag, Au 65 º 48’N 143 º 27’E Okhotsk Zone (Eastern Asia-Arctic Metallogenic Belt) of Au-Ag Epithermal Vein Deposits (mainly Late Cretaceous and early Tertiary), Southeastern Part of Russian Northeast (Belt EAOH) Agat Au-Ag epithermal vein Au, Ag 60 º 58’N 150 º 53’E Aldigych Au-Ag epithermal vein Au, Ag 62 º 19’N 159 º 58’E Burgagylkan Au-Ag epithermal vein Au, Ag 60 º 38’N 146 º 45’E Druchak Au-Ag epithermal vein Ag, Au 62 º 60’N 160 º 03’E Evenskoe Au-Ag epithermal vein Au, Ag 62 º 32’N 159 º 45’E Irbychan Au-Ag epithermal vein Au, Ag 62 º 41’N 159 º 55’E Julietta Au-Ag epithermal vein Au, Ag 61 º 10’N 153 º 59’E Karamken Au-Ag epithermal vein Au, Ag 60 º 14’N 150 º 60’E Kegali Au-Ag epithermal vein Au, Ag 63 º 23’N 161 º 42’E Co
Table 4—Continued Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Khakandzhinskoe (Khakandzha) Au-Ag epithermal vein Au, Ag 60 º 02’N 142 º 36’E Kinzhal Sn silicate-sulfi de vein Sn 62 º 17’N 151 º 58’E Kolkhida Au-Ag epithermal vein Ag, Au, Sn 60 º 37’N 151 º 27’E Krasivoe Au-Ag epithermal vein Au, Ag 59 º 28’N 140 º 22’E Maltan Stock Granitoid-related Au Au, Bi, Te 61 º 28’N 150 º 52’E Nevenrekan Au-Ag epithermal vein Au, Ag 62 º 14’N 159 º 11’E Oira Au-Ag epithermal vein Au, Ag 60 º 09’N 149 º 45’E Olyndja Au-Ag epithermal vein Ag, Au 62 º 26’N 157 º 35’E Senon, Utro, Serebryanoe Epithermal vein and volcanic- Ag, Au, Sb 60 º 40’N 148 º 05’E hosted Sb vein Sentyabr Au-Ag epithermal vein Ag, Au 60 º 44’N 149 º 22’E Skarnovoe Pb-Zn-Ag skarn Zn, Pb, Ag 60 º 46’N 150 º 38’E Spiridonych, Teply Au-Ag epithermal vein Au, Ag 61 º 20’N 156 º 17’E Utessnoe Au-Ag epithermal vein Ag, Au, Hg 60 º 26’N 150 º 41’E Verkhnenyotskoe Au-Ag epithermal vein Au, Ag 58 º 17’N 139 º 06’E Vetvisty Au-Ag epithermal vein Ag, Au 62 º 07’N 152 º 08’E Yurievka Au-Ag epithermal vein Au, Ag 59 º 41’N 141 º 44’E Koni-Yablon Zone (Eastern Asia-Arctic Metallogenic Belt) of Porphyry Cu-Mo and Cu-Mo Skarn Deposits (Cretaceous) Southern Part of Russian Northeast (Belt EAKY) Berezovogor Au-Ag epithermal vein Au, Ag, Pb 65 º 50’N 170 º 08’E Etandzha Porphyry Cu-Mo Cu, Mo 57 º 29’N 138 º 39’E Gora Krassnaya Porphyry Cu-Mo Mo, Cu, Au 66 º 35’N 175 º 31’E Guan-Ti (Arkhimed) Porphyry Mo Mo, W 61 º 30’N 143 º 51’E Ikrimun Porphyry Cu-Mo Cu, Mo 59 º 21’N 146 º 59’E Irgunei Au-Ag epithermal vein Au, Ag 64 º 42’N 166 º 50’E Khakandya Porphyry Mo Mo 60 º 49’N 153 º 32’E Lastochka Mo greisen and vein Mo 64 º 32’N 165 º 07’E Maly Komui Cu skarn Cu 57 º 23’N 137 º 32’E Molybdenitovy Porphyry Mo Mo 61 º 33’N 142 º 59’E Nakhtandjin, Lora Porphyry Cu Cu 59 º 25’N 153 º 29’E Nyavlenga Au-Ag epithermal vein Au, Ag 60 º 44’N 153 º 28’E Osennee, Oksa, Usinskoe Porphyry Cu-Mo Mo, Cu 59 º 44’N 150 º 16’E Sergeev Au-Ag epithermal vein Au, Ag 63 º 52’N 165 º 41’E Serovskoe Au-Ag epithermal vein Au, Ag 65 º 17’N 169 º 00’E Tikas Porphyry Mo Mo 61 º 40’N 161 º 21’E Travka Porphyry Mo Mo 64 º 48’N 168 º 36’E Tsirkovy Granitoid-related Au Au, Ag, Cu, W, Bi 63 º 33’N 165 º 07’E Uralskoe Volcanic-hosted Hg Hg, Sb, Au, Ag 66 º 28’N 166 º 48’E Viking Porphyry Cu-Mo Cu, Mo 58 º 58’N 152 º 34’E Yapon Porphyry Cu Cu 59 º 25’N 154 º 52’E Korkodon-Nayakhan Zone (Eastern Asia-Arctic Metallogenic Belt) of Porphyry Mo and Granitoid-Related Au Deposits (Late Cretaceous), East-Central Part of Russian Northeast (Belt EAKN) Khetagchan Granitoid-related Au Au, W, Bi 63 º 24’N 157 º 04’E Orlinoe Porphyry Mo Mo 62 º 35’N 157 º 16’E Sedoi Ag-Co arsenide vein and Fe-Pb- Ag, Co 63 º 49’N 158 º 25’E Cu-Ag-Au skarn Appendix 385 Skarn Fe (±Au, Cu, W, Sn) skarn Fe 63 º 29’N 158 º 32’E Verkhny-Koargychan Au-Ag Polymetallic vein Au, Ag, Pb, Zn 63 º 07’N 159 º 19’E Verkhne–Kolyma Zone (Eastern Asia-Arctic Metallogenic Belt) of Sn-Ag Polymetallic Vein, (Southern Bolivian type), Sn Polymetallic Vein, Rhyolite-Hosted Sn, and Granitoid-Related Au Deposits (Cretaceous), Southeastern Part of Russian Northeast (Belt EAVK) Aida Au-Ag epithermal vein Ag, Au 63 º 36’N 144 º 01’E Baryllyelakh-Tsentralny Sn polymetallic vein Sn, Ag 63 º 26’N 143 º 48’E Bogatyr Sn silicate-sulfi de vein Sn 61 º 02’N 145 º 55’E Bulunga Pb-Zn-Ag vein or skarn Pb, Zn, Ag 62 º 18’N 145 º 42’E Dneprov Sn silicate-sulfi de vein and Sn greisen Sn 61 º 20’N 151 º 36’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
Page 143 and 144:
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
Page 153 and 154:
The belt is hosted in the Late Jura
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in a island arc that was tectonical
Page 157 and 158:
and Early Cretaceous Koyukuk island
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The deposit consists of disseminate
Page 161 and 162:
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
Page 185 and 186:
Host Granitoid Rocks and Associated
Page 187 and 188:
that are up to 600-1,500 m long, av
Page 189 and 190:
Metallogenic Belts Formed During La
Page 191 and 192:
y partly coeval plutons that range
Page 193 and 194:
tion is interpreted as occuring by
Page 195 and 196:
the Badzhal-Ezop and Khingan parts
Page 197 and 198:
and comagmatic with volcanic rocks;
Page 199 and 200:
as interpreted for the Rock Creek d
Page 201 and 202:
source (Yeo, 1992). The Blow River
Page 203 and 204:
2000). The spatial location of the
Page 205 and 206:
to the east in the central Yukon Te
Page 207 and 208:
occur in a 30-km-long belt along ir
Page 209 and 210:
The Emerald deposit has produced ap
Page 211 and 212:
Metallogenic-Tectonic Model for Ear
Page 213 and 214:
cham oceans were closed, and the Ch
Page 215 and 216:
greisenized Mesozoic granite that i
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composition magmatic bodies (with a
Page 219 and 220:
Page 221 and 222:
to Albian pelecypods (Nokleberg and
Page 223 and 224:
quartz-arsenopyrite-pyrrhotite, pol
Page 225 and 226:
thermally altered to siliceous and
Page 227 and 228:
These ore bodies are as much as 1 m
Page 229 and 230:
Eastern Asia-Arctic Metallogenic Be
Page 231 and 232:
Demin, and Krasilnikov, 1974; Nekra
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10 percent Cu, as much as 0.92 perc
Page 235 and 236:
pyrite, pyrite, galena, sphalerite,
Page 237 and 238:
content decreases with depth, as do
Page 239 and 240:
azdelnoye, (2) porphyry Sn deposits
Page 241 and 242:
Karalveem Au Quartz Vein Deposit Th
Page 243 and 244:
Democrat (Mitchell Lode) Granitoid-
Page 245 and 246:
with high-temperature and high-pres
Page 247 and 248:
chalcocite and covellite and also h
Page 249 and 250:
cum-North Pacific, (2) completion o
Page 251 and 252:
(6) In the Paleocene (about 56 to 6
Page 253 and 254:
sists of cinnabar and metacinnabari
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Eastern Asia-Arctic Metallogenic Be
Page 257 and 258:
groups of deposits are interpreted
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Indian Mountain and Purcell Mountai
Page 261 and 262:
and southeastern Alaska (Moll and P
Page 263 and 264:
Nokleberg and others, 1995a; Bundtz
Page 265 and 266:
g/t Au or 368.2 Au gold. The deposi
Page 267 and 268:
wim Group and altered mafic dikes.
Page 269 and 270:
Mount Nansen porphyry Cu-Mo deposit
Page 271 and 272:
A Map 450 500 550 Cross section Dik
Page 273 and 274:
Cretaceous and early Tertiary conti
Page 275 and 276:
deposits, at Chichagoff and Hirst-C
Page 277 and 278:
others, 1994c, 1997c). The signific
Page 279 and 280:
tonnes grading 0.53 percent Ni, 0.3
Page 281 and 282:
with a 0.25 percent cut-off. The de
Page 283 and 284:
Bulkley Metallogenic Belt of Porphy
Page 285 and 286:
Red Rose W-Au-Cu-Ag Polymetallic Ve
Page 287 and 288:
ish Columbia and consists of severa
Page 289 and 290:
during back-arc extension or transt
Page 291 and 292:
stocks and dikes, is associated wit
Page 293 and 294:
etrograde minnesotaite (Fe talc), F
Page 295 and 296:
Specific Events for Early to Middle
Page 297 and 298:
of fractured and faulted Permian-Tr
Page 299 and 300:
sists of a mineralized fracture zon
Page 301 and 302:
dolomite. Wall rock alteration incl
Page 303 and 304:
elt of late Tertiary plutons that a
Page 305 and 306:
plates that exhibit magnetic anomal
Page 307 and 308:
stages (Petrenko, 1999): (1) In the
Page 309 and 310:
mon. The deposit is of medium size
Page 311 and 312:
Metallogenic-Tectonic Model for Lat
Page 313 and 314:
The origin of the Hg deposits of th
Page 315 and 316:
margin or island-arc tectonic envir
Page 317 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 415: 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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