USGS Professional Paper 1697 - Alaska Resources Library

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378 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Table 4—Continued Francois Lake Metallogenic Belt Porphyry Deposits (Late Jurassic to Early Cretaceous) Southern British Columbia (Belt FL) Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Endako Porphyry Mo Mo 54 º 02’N 125 º 07’W Cariboo Metallogenic Belt of Au Quartz Vein Deposits (Middle Jurassic to Early Cretaceous) Southern British Columbia (Belt CB) Cariboo-Barkerville (Aurum, Mosquito Ck.) (093H 019; 093H 010) Au quartz vein Au 53 º 05’N 121 º 34’W Frasergold (Eureka Peak, Kay, Mac) (093A 150) Au quartz vein Au 52 º 18’N 120 º 35’W Rossland Metallogenic Belt of Au-Ag Polymetallic Vein Deposits (Middle Jurassic) Southern British Columbia (Belt RL) Rossland (Le Roi, War Eagle, etc.) (082FSW 093; 082FSW 097; 082FSW 048; 083FSW068) Au-Ag polymetallic vein Au, Ag 49 º 05’N 117 º 49’W Sheep Creek Area (Kootenay Belle, etc.) Au-Ag polymetallic vein Au, Ag, Pb, Zn 49 º 08’N 117 º 08’W Ymir-Erie Creek (Yankee Girl) Au-Ag polymetallic vein Au, Ag 49 º 18’N 117 º 11’W EARLY CRETACEOUS (Neocomian—144 to 120 Ma) Samarka Metallogenic Belt of W Skarn, and Porphyry Cu-Mo Deposits (Early Cretaceous) West-Central Part of Russian Southeast (Belt SA) Benevskoe W skarn W 43 º 06’N 133 º 43’E Kafen Porphyry Cu-Mo Cu, Mo 47 º 36’N 136 º 15’E Khvoshchovoe Porphyry Cu-Mo Cu, Mo 47 º 58’N 136 º 11’E Lermontovsky W skarn and greisen W 46 º 57’N 134 º 27’E Malakhitovoe Porphyry Cu-Mo Cu, Mo 47 º 06’N 135 º 04’E Skalistoe Porphyry Mo Mo 43 º 36’N 133 º 45’E Skrytoe W skarn W 45 º 05’N 134 º 35’E Vostok-2 W skarn W 46 º 28’N 135 º 53’E Algama Metallogenic Belt of Stratiform Zr Deposits (mid-Cretaceous?), Northern Part of Russian Southeast (Belt AL) Algaminskoe Stratiform Zr Zr 58 º 40’N 135 º 34’E Kondyor Metallogenic Belt of Zoned Mafi c-Ultramafi c PGE-Cr Deposits (mid-Cretaceous?) Northern Part of Russian Southeast (Belt KO) Kondyor Zoned mafi c-ultramafi c Cr-PGE Pt 57 º 33’N 134 º 38’E Selemdzha-Kerbi Metallogenic Belt of Au Quartz Vein Deposits (Late Jurassic and Early Cretaceous) Northwestern Part of Russian Southeast (Belt SK) Afanas’evskoe Au quartz vein Au 52 º 50’N 133 º 24’E Ingagli Au quartz vein Au 53 º 04’N 133 º 22’E Kharga Au quartz vein Au 52 º 57’N 133 º 38’E Malomyr Au quartz vein Au 53 º 06’N 131 º 50’E Poiskovoe Granitoid-related Au Au 53 º 08’N 132 º 12’E Sagurskoe Au quartz vein Au 52 º 59’N 132 º 36’E Talaminskoe Sb-Au vein Sb, Au 52 º 42’N 133 º 24’E Tokur Au quartz vein Au 53 º 09’N 132 º 49’E Zazubrinskoe Au quartz vein Au 53 º 09’N 132 º 22’E Stanovoy Metallogenic Belt of Granitoid-related Au Deposits (Cretaceous?) Northern Part of the Russian Southeast (Belt ST) Bamskoe (Chul’bango) Au-Ag epithermal vein Au, Ag 55 º 59’N 123 º 54’E Burindinskoe Au-Ag epithermal vein Au, Ag 53 º 41’N 124 º 54’E Kirovskoe Granitoid-related Au Au 54 º 27’N 124 º 14’E Zolotaya Gora Au quartz vein Au 54 º 19’N 126 º 44’E Kular Metallogenic Metallogenic Belt of Au Quartz Vein, Granitoid-Related Au, Au-REE Quartz Vein, and Sn Quartz Vein Deposits (Early Cretaceous), Northern Part of Eastern Siberia (Belt KU) Burguat Au quartz vein Au 70 º 42’N 134 º 31’E Dzhuotuk Au quartz vein Au 70 º 13’N 134 º 17’E
Table 4—Continued Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Novoe Granitoid-related Au Au 69 º 36’N 133 º 07’E Solur Granitoid-related Au Au 70 º 01’N 133 º 24’E Tirekhtyak district (Nagornoe, Sn quartz vein Sn, W 69 º 58’N 134 º 41’E Podgornoe, Poputnoe) Allakh-Yun Metallogenic Belt of Au Quartz Vein Deposits and Associated W-Sn Quartz Vein Deposits (Late Jurassic to Early Cretaceous), Southern Part of Russian Northeast (Belt AY) Bular Au quartz vein Au 61 º 13’N 137 º 50’E Burgali Porphyry-Mo (W) Mo, W 59 º 56’N 138 º 51’E Dies Cu skarn Cu 59 º 10’N 138 º 11’E Duet Au quartz vein Au 59 º 48’N 137 º 44’E It-Yuryak W vein, Sn (W)-quartz vein W 62 º 42’N 139 º 38’E Levo-Dybin Granitoid-related Au Au, W, Bi 62 º 50’N 139 º 35’E Malyutka Au quartz vein Au 58 º 38’N 137 º 16’E Muromets Cu-Mo skarn Cu, Mo, W 58 º 48’N 137 º 38’E Nezhdaninka Au quartz vein Au, Ag 62 º 34’N 139 º 19’E Novinka Au quartz vein Au 61 º 42’N 138 º 17’E Onello (Lider) Au quartz vein Au 62 º 23’N 137 º 52’E Svetly Au quartz vein Au 61 º 28’N 137 º 19’E Voskhod Au quartz vein Au 61 º 22’N 139 º 22’E Yur Au quartz vein Au 59 º 55’N 137 º 48’E Yana-Polousnen Metallogenic Metallogenic Belt of Granitoid-Related Sn Quartz Vein, W Vein, Sn Greisen, Co-, Au-, and Sn-Skarn, Sn-Silicate Sulfi de Vein and Related Deposits (Early Cretaceous), Central Part of Russian Northeast (Belt YP) Altinskoe Polymetallic vein Pb, Zn 69 º 47’N 142 º 14’E Alys-Khaya Sn polymetallic vein Sn 65 º 56’N 135 º 43’E Anomalnoe Sn silicate-sulfi de vein Sn 65 º 37’N 131 º 49’E Aragochan Polymetallic vein Pb, Zn 69 º 44’N 137 º 00’E Arbatskoe Co skarn Co 69 º 28’N 149 º 41’E Argin Sn quartz vein Sn 68 º 03’N 135 º 50’E Balyktaah, Ploskoe Sn greisen Sn 69 º 50’N 151 º 48’E Bugdogar Sn polymetallic vein Sn 65 º 12’N 133 º 59’E Burgachan Sn polymetallic vein Sn 65 º 46’N 134 º 45’E Chistoe Granitoid-related Au Au 69 º 43’N 150 º 15’E Dalnee Polymetallic vein Pb, Zn 69 º 49’N 138 º 30’E Dokhsun Polymetallic vein Pb, Zn, Cu 69 º 26’N 144 º 27’E Ege-Khaya Sn polymetallic vein Sn, Zn 67 º 38’N 134 º 47’E Ilin-Tas Sn silicate-sulfi de vein Sn 65 º 60’N 135 º 56’E Kandidatskoe Au skarn Au, Co, As 69 º 24’N 149 º 44’E Kester Sn greisen Sn, Ta, Nb, Li 67 º 17’N 134 º 38’E Khoton-Khaya Sn-polymetallic vein, Sn silicate- Sn 67 º 17’N 133 º 47’E sulfi de vein Polyarnoe Sn greisen and vein Sn, W 69 º 37’N 141 º 45’E Takalkan Sn greisen Sn 68 º 59’N 139 º 44’E Tuguchak-1 Mo quartz vein Mo 69 º 30’N 149 º 19’E Tuguchak-2 Granitoid-related Au Au, W, Bi, Te 69 º 30’N 149 º 19’E Ulakhan-Egelyakh Sn silicate-sulfi de vein Sn 67 º 09’N 134 º 21’E Ulakhan-Sala Sn silicate-sulfi de vein Sn 69 º 48’N 136 º 40’E Verkhne-Naanchan Polymetallic vein Pb, Zn 69 º 39’N 150 º 41’E Darpir Metallogenic Belt of Sn and Associated Felsic-Magmatism Deposits (Early Cretaceous) Western Part of Russian Northeast (Belt DP) Bastion Sn greisen Sn 63 º 17’N 153 º 13’E Bolshoy Kanyon Sn skarn Sn 63 º 15’N 151 º 05’E Chepak Granitoid-related Au Au, W, Bi 63 º 05’N 152 º 45’E Chibagalakh Sn-B skarn B, Sn 68 º 13’N 139 º 51’E Darpir Sn silicate-sulfi de vein Sn 64 º 02’N 147 º 42’E Lazo Sn silicate-sulfi de vein Sn 63 º 12’N 152 º 13’E Titovskoe Sn (B) magnesian skarn B 67 º 33’N 139 º 14’E Appendix 379
Page 1 and 2:
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
Page 187 and 188:
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;
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
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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
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quartz-arsenopyrite-pyrrhotite, pol
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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
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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
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
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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
Page 255 and 256:
Eastern Asia-Arctic Metallogenic Be
Page 257 and 258:
groups of deposits are interpreted
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Indian Mountain and Purcell Mountai
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and southeastern Alaska (Moll and P
Page 263 and 264:
Nokleberg and others, 1995a; Bundtz
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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: 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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