40 Metallogenesis and Tectonics of the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera Margin (NSV) were the Kotelnyi (KT), Omulevka (OV), Prikolyma (PR), Nixon Fork-Dillinger-Mystic (NX, DL, MY), Viliga (VL), and Zolotogorskiy (ZL) passive continental-margin terranes, the Avekova (AK), Kilbuck-Idono (KI), Okhotsk Position unknown. Possible derivation from Barents Sea region. ? WRA (AX) NSC EARLY MISSISSIPPIAN RIFTS SD, KR (OK) BE BE 0 800 km 0 800 mi NSC NSV, KN (KT) GL OL KEYA KEDON ARC WRA (AX) SICKER ARC (AK) 40 MS (VL) o YR ? UNK (OV) (OM) (KI) ANGAYUCHAM OCEAN 14 o (NX, DL, MYMY) (PR) NAM (SD) UNK (OK), and Omolon (OM) cratonal terranes. Derived from the Devonian continental-margin arc that formed along the margins of the North Asian Craton Margin were the Beryozovka (BE), Oloy (OL), and Yarakvaam (YA) terranes (fig. 18). The SEL TO EARLY MISSISSIPPIAN SINISTRAL-SLIP FAULT AND RIFT (ZL) AT PRE-DEVONIAN DEXTRAL-SLIP SUTURE URS (RA) ? AKY (CO) NAC (AA) (RB) ANCESTRAL PACIFIC OCEAN DE DA BR NCO MP 0 o (KO) NAC LATE DEVONIAN & EARLY FL GA MISSISSIPPIAN (YT) RL RIFT SRM FR TR UNK 387 to 360 Ma. METALLOGENIC BELTS AKY - <strong>Alaska</strong> Range & Yukon-Tanana Upland AT - Arctic BE - Berezovka River BR - Brooks Range DE - Dempster FL - Finlayson Lake FR - Frances Lake GA - Gataga KE - Kedon KR - Khamna River KS - Kootenay-Shuswap MP - Macmillan Pass MS - Mount Sicker MY - Mystic NBR - Northwestern Brooks Range NCO - Northern Cordillera RL - Robb Lake SD - Sette-Daban SEL - Selennyakh River SRM - Southern Rocky Mountain TR - Tracy TO - Tommot River URS - Urultun & Sudar Rivers YA - Yaroslavka Figure 18. Middle through Late Devonian (387 to 360 Ma) stage of metallogenic-tectonic model for the Russian Far East, <strong>Alaska</strong>, and the Canadian Cordillera and adjacent offshore areas. Refer to text for explanation of metallogenic-tectonic events and to tables 3 and 4 for descriptions metallogenic belts and significant deposits. Adapted from Nokleberg and others (1997b, 1998, 2000). KS NAM ?
newly created terranes migrated into the Angayucham Ocean. Derived from the North American Craton Margin (NAM) were the Kootenay (KO) and Yukon-Tanana (YT) passive continental-margin terranes. The following metallogenic belts, which contain massive sulfide, carbonatite-related Nb, Ta, and REE, or related deposits, formed during rifting: Berezovka River (BE); Cathedral (CA), Dempster (DE), Finlayson Lake (FL); Gataga (GA), Ingenika (IN), Liard (LI), older part of Mystic CRATON MARGIN TECTONIC ENVIRONMENTS AND GEOLOGIC UNITS EXPLANATION CRATONAL Cratons (No patterns) : NAC , North American; NSC , North Asian; NSS, Stanovoy block; Terranes: AK, Avekova; GN, Gonzha; KI , Kilbuck-Idono; OK, Okhotsk; OM, Omolon CONTINENTAL-MARGIN ARC, ISLAND ARC, OR TURBIDITE BASIN (Subduction-related; includes forearc and backarc, and related turbidite basin deposits) SUBDUCTION-ZONE OR ACCRETIONARY-WEDGE COMPLEX OR OPHIOLITE BACKARC SPREADING OR HOT-SPOT UNITS OCEANIC Craton Margins: NAM, North American; NSV, North Asian (Verkhoyansk foldbelt; NSS, North Asian (Stanovoy block) Passive continental-margin terranes (derived from craton margins): AA, Arctic <strong>Alaska</strong>; AP, Artis Plateau; CA, Cassiar; CH, Chukotka; CK, Chukchi Cap; CO, Coldfoot; CS, Chukchi Spur; DL, Dillinger; KN, Kula-Nera; KO, Kootenay; KT, Kotel’nyi; LO, Lomonosov; MY, Mystic; NR, Northwind Ridge; NX, Nikon Fork; OL, Oldoi; OV, Omulevka; PC, Porcupine; PR, Prikolyma; RA, Rassokha; RB, Ruby; SD, Seward; SR, Sredinny-Kamchataka; VL, Viliga; WS, Wickersham; YT , Yukon-Tanana; ZL, Continental-margin arcs: al, Aleutian; at, <strong>Alaska</strong> Range-Talkeetna Mountains; bw, Bowers Ridge; ca, Cascade; ck, Central Kamchatka; cn, Coast-North Cascade; ej, East Japanl; ek, East Kamchatka; es, East Sikhote-Alin; gg, Gravina-Nutzotin-Gambier; io, Indigirka-Oloy; ka, Kamloops; kc, Central Kamchatka; kk, Kamchatka-Koryak; kh, Kahiltna; km, Kuskokwim Mountains; ko, Khingan-Okhotsk; ku, Kuril; mo, Monakin; no, North Okhotsk; oc, Okhotsk- Chukotka; ol, Oloy; os, Oloy-Svyatov Nos; pn, Penzhina; ns Nelson; sb Spences Bridge; sh Shirshov Ridge; sv, Svyotoy-Nos; tt, Tahtsa-Twin Sisters- Francois Lake; ud, Uda; uo, Umlekan-Ogodzhin; wk, West Kamchatka; wr, Wrangell Terranes: AL, Alazeya; AX, Alexander; BE, Beryozovka; BU, Bureya; CD, Cadwallader; CK, Chilliwack River; IR, Iruneisky; IZ, Izee; KE, Kema; KH, Khetachan; KLO, Kolyma-Omolon superterrane; KM, Kony-Murgal; KRO, Kronotskiy; KT, Kotel’nyi; KY, Koyukuk; LA, Lan; LD, Laoelin-Grodekorsk; MAI, Mainitskiy; MT, Methow; NE, Nemuro; NU, Nutesyn; NY, Nyac; PE, Peninsula; OF, Olds Ferry; OKA, Olyutorka-Kamchatka; OL, Oloy; QN, Quesnellia; SB, Stobolvskoy; SG, Sergeevka; SH, Shmidt; ST, Stikinia; SY, Sorachi-Yezo; TG, Togiak; TR, Terpeniya; UB, Uniya-Bom; WA, Wallowa; WP, West Pekul’ney; WR, Wrangellia; WRA, Wrangellia superterrane; WSA, West Sakhalin; YA, Yarakvaam AG, Angayucham; AM, Amur River; AC, Aluchin; AGR, Argatas; ANV, Aniva; AV, Alkatvaam; BA, Baker; BD, Badzhal; BR, Bridge River; CC, Cache Creek; CG, Chugach; DB, Debin; EA, Easton; EK, Ekonay; GB, Garbyn’ya; GD, Goodnews; GL, Galam; GS, Grindstone; HI, Hidaka; HO, Hoh; KB, Khabarovsk; KK, Kamuikotan; KLM, Kiselevka-Manoma; KN, Kula Nera; KUK, Kuril-Kamchatka; MU, Munilkan; NAB, Nabilsky; OC, Olympic Core; OS, Oshima; PA, Penzhina- Anadyr; PK, Pekul’ney; PR, Pacific Rim; PW, Prince William; SA, South Anyui; SM, Slide Mountain; SMA, Samarka; SV, Seventymile; SZ, Siletzia; TD, Turkuringra-Dzhagdi; TL, Talovskiy; TO, Tokoro; TR, Terpeniya; TU, Taukha; UL, Ulban; UNK, Unknown; VE, Velmay; VT, Vetlovskiy; WK, West Kamchatka; YAK, Yakutat; YN, Yanranay am, Alpha and Mendeleev Ridges; bs, Bering Sea; cr, Columbia River; kr, Kuril; sj, Sea of Japan; sp, Sakhalin-Primorye Plates: FAR, Farallon; JF, Juan de Fuca; KULA, Kula; PAC, Pacific; EX, Explorer; Oceanic ridges: GK, Gakkel; JFR, Juan de Fuca; KOM, Komandorsky POST-ACCRETION OVERLAP SEDIMENTARY AND VOLCANIC UNIT, SUBMARINE FAN, OR OCEAN BASIN DEPOSIT ab, Amerasia Basin; ar, Anadyr; atb, Aleutian-Bowers; bo, Bowser; bu, Bureya; cb, Canada Basin; cf, Cordilleran Foreland; co, Colville; eb, Eurasia Basin; kb, Kuibiveem; kn, Kandik River; kw, Kuskokwim COLLAGE OF PREVIOUSLY ACCRETED TERRANES AND EXTINCT TERRANES, OVERLAP ASSEMBLAGES, AND BACKARC UNITS (names of units in parentheses) COLL, Collages of various accreted terranes (some labeled); ASC, Academy of Sciences; IOC, Institute of Oceanology; KT, Kotel’nyi; TA, Taymyr Peninsula Figure 18.—Continued. Middle and Late Devonian Metallogenic Belts (387 to 360 Ma; figures 16, 17) 41 (MY), Northern Cordillera (NCO), Macmillan Pass (MP), Robb Lake (RL), Selennyakh River (SEL), Sette-Daban (SD), Southern Rocky Mountain (SRM), Tommot River (TO), Urultun and Sudar Rivers (URS), and Yarkhodon (YR). (4) The Sicker island arc was active along most of the length of the Wrangellia superterrane (WRA), which at this time was composed only of the Alexander sequence (AX) of the Wrangellia superterrane. Associated with the Sicker arc B B CONTACTS AND FAULTS (Dashed where concealed or approximately located; querried where unknown) Contact DE (cb) 14 o Thrust fault, barbs on upper plate Strike-slip fault Regional continental-rift. Barbs towards extended area Subduction zone, barbs point toward subducting margin Transform fault along oceanic ridge SYMBOLS Oceanic ridges: GK, Gakkel; JFR, Juan de Fuca Backarc spreading, barbs face spreading basin Zone of active metamorphism and deformation of continental margin Zone of blueschist-facies metamorphism Fault name abbreviation Abbreviations for extensive extinct basin, previously accreted terranes, or inactive arcs in parentheses Direction of tectonic migration or major oroclinal bending Paleopole Paleolatitude PLUTONIC BELTS Collisional granite belts: ma, Main; no, Northern; om, Omineca-Selwyn; tr, transverse; wvk, West Verkhoyansk Subduction-related continental-margin plutonic rocks Oceanic-ridge-related plutonic rocks: sab, Sanak-Baranof plutonic belt FAULT NAMES AD Adycha-Taryn AL Aleutian megathrust CA Central Sikhote-Alin CC Cascadia megathrust CO Contact DE Denali FS Frasier-Straight Creek HA Harrison KA Kaltag KE Ketanga KK Kuril Kamchatka megathrust KO Kobuk-South Fork LE Lena Boundary of neotectonic block defined by modern seismicity METALLOGENIC BELT OH Relative direction and motion of oceanic plate and continental plates with respect to North American or North Asian Cratons LS Lyakhov-South Anyui MO Mongol-Okhotsk MY Myatisk NF Nixon Fork RL Ross Lake QC Queen Charlotte- Fairweather SH Sakhalin-Hokkaido TE Teslin TI Tintina UL Ulban UM Ulakhay Metallogenic belt with abbreviation
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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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- Page 43 and 44: 2 to 20 m thick. A related dolomite
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- Page 53 and 54: Monashee Metallogenic Belt of Sedim
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- Page 57 and 58: in addition to the Fe deposits. Min
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- Page 79 and 80: mafic and felsic metavolcanic rocks
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- Page 95 and 96: Berezovka River Metallogenic Belt o
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- Page 105 and 106: (NX, DL, MY), Viliga (VL), and Zolo
- Page 107 and 108: South of the main east-west-trendin
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- Page 115 and 116: Viliga (VL) passive continental-mar
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- Page 119 and 120: superterrane, consists mainly of ma
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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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Origin of and Tectonic Controls for
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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
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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
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Manns, F.T., 1981, Stratigraphic as
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Miller, M.L., and Bundtzen, T.K., 1
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Mortimer, N., 1987, The Nicola Grou
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Noble, S.R., Spooner, E.T.C., and H
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Canada Annual Meeting, Saskatoon, S
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Perello, J.A., Fleming, J.A., O’K
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Far East—Mineralogical criteria f
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Roeske, S.M., Mattinson, J.M., and
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Schmidt, J.M., and Zierenberg, R.A.
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formation occurrences: Materialy po
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Struik, L.C., 1986, Imbricated terr
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Valuy, G., and Rostovsky, F., 1988,
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Wolfe, W.J., 1995, Exploration and
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Appendix Table 1. Mineral deposit m
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Table 2 Summary of correlations and
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Table 2—Continued Unit(s) and Cor
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Table 2—Continued Unit(s) and Cor
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 3—Continued Metallogenic Be
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Table 4. Significant lode deposits,
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Table 4—Continued Appendix 369 De
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Table 4—Continued Tracy Metalloge
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Table 4—Continued Appendix 373 In
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Table 4—Continued Deposit Name Mi
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Table 4—Continued Mainits Metallo
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Table 4—Continued Deposit Name Mi
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Table 4—Continued Appendix 381 De
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Table 4—Continued Whitehorse Meta
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Table 4—Continued Deposit Name Mi
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Table 4—Continued Appendix 387 De
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Table 4—Continued Appendix 389 LA
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Table 4—Continued Deposit Name Mi
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Table 4—Continued Surprise Lake M
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Table 4—Continued Sredinny Metall
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Table 4—Continued Deposit Name Mi