USGS Professional Paper 1697 - Alaska Resources Library

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Table 3—Continued Metallogenic Belt Major Mineral Deposits Types. Environment and Tectonic Event and (Abbreviation) (Signifi cant Mineral Deposits) Host Unit Comments LATE TERTIARY and QUATERNARY METALLOGENIC BELTS (Pliocene through Present—4 to 0 Ma) (fi gs. 17, 18) Metallogenic Belts Formed in Late Tertiary and QuaternaryContinental-Margin Arcs, Kamchatka Peninsula, Southern Alaska, and Southern Canadian Cordillera Sakhalin Island (SH) Silica-carbonate, volcanic-hosted Hg Rear of a continental-margin Back-arc spreading behind Kuril arc? deposits. arc? (In’ River, Inskoe Ostrinskoe, Svetlovskoe , Yasnoe) Shear zones. Metallogenic Belt Major Mineral Deposits Types. Environment and Tectonic Event and (Abbreviation) (Signifi cant Mineral Deposits) Host Unit Comments Kuril (KU) Au-Ag epithermal vein, polymetallic Continental-margin arc. Subduction-related granitic plutonism that formed the Kuril Island part of vein, Sn vein, sulfur-sulfi de, & others. (Novoe, Prasolovskoe, Koshkina, Valentinovskoe) Kuril volcanic-plutonic belt. Northeast Asia continental margin arc. Alaska Peninsula & Aleutian Islands (AP) Continuing Metallogenic Belts Belt started in Miocene. Owl Creek (OC) Belt started in Eocene. 366 Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera
Table 4. Significant lode deposits, locations, and major metals for major Proterozoic and Phanerozoic metallogenic belts in the Russian Far East, Alaska, and the Canadian Cordillera. [Refer to figures 2-18 for location of metallogenic belts. For each time interval (time-stage), metallogenic belts are listed in a clockwise order, according to similar tectonic environments, starting with the area of the Russian Southeast and ending with the area of the southern Canadian Cordillera. Attributes of lode deposits and characteristics of metallogenic belts are defined and adapted from Nokleberg and others (1997a,b, 1998b) and as modified herein. Abbreviations given for metallogenic belts as depicted on generalized maps of metallogenic belts and host rocks and on metallogenic-tectonic model for Devonian through Present. For each metallogenic belt, mineral deposits listed in alphabetical order. Most major mineral deposits for the Yukon Territory (northwest Canadian Cordillera) have deposit numbers from the MINFILE of the Yukon Geological Survey (Dekelerk, 2002) listed in parens after the deposit name. These deposits descriptions can be accessed from the Yukon Geological Survey MINFILE Web site at: http://www.geology.gov.yk.ca/minfile/. Most major mineral deposits for British Columbia (southwest Canadian Cordillera) have deposit numbers from MINFILE (2002) listed in parens after the deposit name. These deposit descriptions can be accessed from the MINFILE Web site at www.em.gov.bc.ca/mining/geolsurv/minfile/.] Appendix 367 PROTEROZOIC (2500 TO 570 Ma) Oroek Metallogenic Belt of Ironstone and Sediment-Hosted Cu Deposits (Middle and Late Proterozoic) West-Central Part of Russian Northeast (Belt OK) Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Oroek Sediment-hosted Cu Cu 64 º 54’N 152 º 48’E Pobeda Ironstone Fe 65 º 43’N 152 º 12’E Lantarsky-Dzhugdzhur Belt of Anorthosite Apatite-Ti-Fe and Gabbroic Ni-Cu (PGE) Deposits (Mesoproterozoic), Southern Part of Russian Northeast (Belt LD) Bogidenskoe Anorthosite apatite Ti-Fe Ti, P 55 º 38’N 133 º 42’E Dzhaninskoe Anorthosite apatite Ti-Fe Ti, P 55 º 31’N 134 º 09’E Gayumskoe Anorthosite apatite Ti-Fe Ti, P 55 º 43’N 134 º 15’E Maimakanskoe Anorthosite apatite Ti-Fe Ti, P 55 º 37’N 134 º 30’E Avlandzhinsky, Kontaktovy, Nyandomi, Odorin, Ozerny. Gabbroic Ni-Cu Cu-Ni-Co-PGE Cu, Ni, PGE 58 º 08’N 137 º 55’E Ulkan Metallogenic Belt of Felsic Plutonic REE Deposits (Mesoproterozoic), Southeastern Part of Russian Northeast (Belt UL) Ulkanskoe Felsic plutonic REE REE, Be, Zr 56 º 19’N 134 º 49’E Bilyakchan Metallogenic Belt of Sediment-hosted Cu and basalt Cu Deposits (Mesoproterozoic and Neoproterozoic), Southeastern Part of Russian Northeast (Belt BI) Dzhagdag Basaltic Cu Cu 57 º 22’N 137 º 13’E Omolon Metallogenic Belt of Ironstone (Superior Fe) Deposits (Archean to Early Proterozoic) Central Part of Russian Northeast (Belt OM) Verkhny-Omolon Ironstone Fe 63 º 21’N 158 º 22’E Kilbuck Metallogenic Belt of Ironstone (Superior Fe) Deposits (Early Proterozoic), Southwestern Alaska (Belt KI) Canyon Creek Ironstone Fe 59 º 38’N 161 º 08’W Sinuk River Metallogenic Belt of Stratiform Massive Sulfi de-Barite and Stratabound Fe and Mn Deposits (Late Proterozoic or older), Western Alaska (Belt SR) Aurora Creek Kuroko massive sulfi de? Zn, Pb, Cu, Ba, Ag, Au 64 º 46’N 164 º 58’W American, Bear, Cub, Monarch Stratabound Fe-Mn Fe, Mn, F 64 º 48’N 165 º 24’W Gillespie Metallogenic Belt of SEDEX Pb-Zn Deposits (Early Proterozoic), Yukon Territory (Belt GE) Blende Sedimentary exhalative Pb-Zn Zn, Cu, Pb, Au, Ag 64 º 25’N 134 º 30’W Hart River Sedimentary exhalative Zn-Cu-Pb Zn, Cu, Ag 64 º 39’N 136 º 51’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
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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
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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
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Bazard, D.R., Butler, R.F., Gehrels
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Bradley, D.C., Haeussler, P.J., and
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Bundtzen, T.K., Laird, G.M., Caluti
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Cecile, M.P., 1982, The lower Paleo
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Debari, S.M., and Coleman, R.G., 19
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U.S. Bureau of Land Management Open
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Cordilleran Orogen in Canada: Geolo
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Goldfarb, R., Hart, C., Miller, M.,
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Grove, E.W., 1986, Geology and mine
Page 337 and 338:
Høy, T., 1982a, Stratigraphic and
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Jones, D.L., Silberling, N.J., Cone
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Kutyev, F. Sh., Baikov, A.I., Sidor
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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 397: Table 3—Continued Metallogenic Be
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 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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