Metallogenesis and Tectonics of the Russian Far East, Alaska, and ...

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Metallogenic Belt (Abbreviation) Alaska Range and Yukon-Tanana Upland (AKY) Dawson (DA) Frances Lake (FR) Tracy (TR) Mount Sicker (MS) Kootcnay-Shuswap (KS) Major Mineral Deposits Types. (Significant Mineral Deposits) Kuroko massive sulfide. (WTF, Red Mountain, Sheep Creek, Liberty Bell, Anderson Mountain, Miyaoka, Hayes Glacier, McGinnis Glacier, Delta district) Volcanogenic Pb-Zn-Cu Massive sulfide, SEDEX Pb-Cu-Zn-Ba (Lucky Joe, Mickey, Lone Star) Kuroko massive sulfide. (Kudz Ze Kayah, Wolverine-Lynx) Environment. Host Unit. Continental-margin arc. Yukon-Tanana terrane. Continental-margin arc. Yukon-Tanana terrane. Continental-margin arc. Yukon-Tanana terrane. Tectonic Event. Comments Subduction-related volcanism associated with Late Devonian and Mississippian submerged continental-margin arc. Arc and metallogenic belt extended into early Mississippian. Arc formation succeeded by continental-margin rifting. Subduction-related volcanism associated with Late Devonian and Mississippian submerged continental-margin arc. Arc and metallogenic belt extcnded into early Mississippian. Arc formation succeeded by continental-margin rifting. Subduction-related volcanism associated with submerged continental-margin arc. Arc and metallogenic belt extended into early Mississippian. Arc formation succeeded by continental-margin rifting. Subduction-related volcanism associated with submerged continental-margin arc. Kuroko massive sulfide. Continental-margin arc. (Ecstall, Alamo, Sweetheart Ridge, Yukon-Tanana terrane (pre- Sumdum, & others) rift). Kuroko volcanogenic massive sulfide. Island arc. Subduction-related volcanism associated with island arc. (Mount Sicker (Lenora-Tyee, Twin J, Lara, Coppcr Canyon); Myra Falls (Lynx, Myra, Price, HW)) Wrangellia superterrane. Kuroko, Besshi, and Cyprus massive Back-arc part of continental- Subduction-rclated volcanism associated with submcrgcd continental-margin arc. sulfide. margin arc. Belt extended into early Mississippian. Arc formation succeeded by continental- (Shuswap, Goldstream, Harper Creek, Chu Chua, Adams, Liard, & others) Kootenay terrane (pre-rifting) margin rifting. Metallogenic Belts Formed During Middle Paleozoic Rifting of North Asian Craton Margin Khalnna River (KR) I Carbonatite-related Nb, Ta, REE. I Rifted passive continental I Rifting of middlc Paleozoic (Devonian) continental-margin. Hosted in Late I (Kharnna. Gornoe Ozero) I margin. I Devonian alkalic granitic rocks and carbonatitcs. I ~orth ~sian Craton Margin. Sette-Daban (SD) I Southeast Missouri Pb-Zn, sediment- I Rifted passive continental I Rifting of middle Paleozoic (Late Devonian to Early Mississippian) contincntal- I hosted Cu. I margin. I margin. Belt continued into Early Mississippian. Selennyakh Rivcr (SEL) Tommot River (TO) Unlltun & Sudar Rivers (URS) Yarkhodon (YR) (Sardana, Urui, Kupandzha) Southeast Missouri Pb-Zn, stratabound Hg. (Gal-Khaya, Kondakovskoe) Carbonatite-related Nb, Ta. and REE (Tommot) Southeast Missouri Pb-Zn, carbonatchosted Hg. (Urultun, Uochat) Southeast Missouri Pb-Zn (Slezovka, Gomoc) North Asian Craton Margin. Rifted passive contincntal margin. Omulevka terrane. Rifted passive continental margin. Omulevka terrane. Rifted passivc continental margin. Omulevka terrane. Rifted passive continental margin. Rifting of middle Paleozoic (Late Devonian to Early Mississippian) continental- margin. Belt continued into Early Mississippian. Rifting of middle Paleozoic (Late Devonian to Early Mississippian) continental- margin. Bclt continued into Early Mississippian. Rifting of middlc Paleozoic (Latc Devonian to Early Mississippian) continental- margin. Bclt continued into Early Mississippian. - - - - - - - - - - -- - Rifting of middle Paleozoic (Late Devonian to Early Mississippian) continental- margin. Belt continued into Early Mississippian.
Metallogenic Belt (Abbreviation) Berezovka River (BE) Major Mineral Deposits Types. (Significant Mineral Deposits) Kuroko massive sulfide and sulfide vein. (Berezovskoe) Environment. Host Unit. Rifted passive continental margin. Berezovka terrane. (Leguil Creek, Lower Liard) American continental-margin. Tectonic Event. Comments Rifting of middle Paleozoic (Late Devonian to Mississippian) continental-margin. Belt continued into Permian(?). North American Continental Margin. Belt extended from Late Proterozoic to -
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I EUSGS science Ior a changing wwld
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CONTENTS Abstract .................
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5 : 3 . Kedon metall lo genic Belt
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Parson and Brisco Barite Vein and G
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Overview ..........................
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Chepak Granitoid-Related Au Deposit
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Origin of and Tectonic Controls for
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Au-Ag Epithermal Vein Deposits Asso
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Metallogenesis and Tectonics of the
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and Byalobzhesky (1996). A volume c
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1,079 significant mineral deposits
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Acknowledgements We thank the many
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0 --mmm=oRuwrrrur ommmmarUaAll NEr-
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Figure 3. Generalized map of mtljor
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Archean granulite facies metamorphi
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Figure 5. Oroek sediment-h section
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1 a a - --rich sandstone ~b-Qmg@ner
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Origin of and Tectonic Setting for
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occur in clastic and impure carbona
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Figure 7. Sullivan sedimentary-exha
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I 1997a, b, 1998). The massive sulf
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Ma which locally form extensive plu
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Figure 10. Gerbikanskoe vdcanogenic
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from crystalline basement of craton
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Figure 13. Howards Pass sedknenWy e
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McLean Arm Porphyry Cu-Mo District
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[..'......I Surfia'al deposits (Hol
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Figwe 16. GeneraCied map of major M
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.- *.-* *. . - - ---- -A - EARLY MI
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Metallogenic Belt Formed During Col
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several tens of meters to 1,300 m l
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Goldfarb (197) who interprets that
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WTF and Red Mountain Kuroko Massive
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interpreted by and as part of a ext
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Mount Sicker Metallogenic Belt of K
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interpreted as vents. The deposit c
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hosted in the Yarkhodon subterrane
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origin of the younger Triassic(?) B
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Mississippian age of mineralizalioi
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Monger and Nokleberg, 1996; Noklebe
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1997a, b). Most of the magnesite an
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FL - Finlayson Lakm FR-FmLake LI -
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disseminations in chert, disseminat
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U F~gure 32 GemMzed m p of mejw -ni
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terrane, and by the Stikine Assembl
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Metallogenic-Tectonic Model for Lat
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. I . r ; 4 ~ (9) During subduction
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Eastern Alaska Range Metallogenic B
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individual flows range from 5 cm to
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occurrence of turbiditic clastic ro
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along the with tectonically-related
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: m- 3- w43 k M- u m u~u) mtl 'M~!A
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island-arc volcanic rocks of the Ni
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-- - //// EpldoW Figure 41. Nickel
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(TC), and Toodoggone (TO) belts whi
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(4) The Angayucham Ocean (Kobuck Se
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lueschist units and the McHugh Comp
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Figure 46. Lawyers Au-Ag epitiefmel
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(5) The Angayucham Ocean (Kobuck Se
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Figure 49 Generaltzed map Of mbjm L
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continental-margin terranes which w
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Pokrovskoe Au-Ag Epithermal Vein De
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Granite-porphm and wanits W e ~~ hl
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subordinate adularia, dolomite, cel
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shale, basalt, plagiorhyolite, silt
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ocks and serpentinite which occur a
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interpreted as forming in the Juras
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Fault / Figure 57. Bond Creek and O
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Klukwan-Duke Metallogenic Bett of M
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tonnes of ore mined between 1967 an
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Cariboo Metallogenic Belt of Au Qua
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Sheep Creek Au-Ag Polymetallic Vein
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---. .% of the North American Conti
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- OwiapaasembC Cmhmmmand Cemmcl. an
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in the west-central part of the Rus
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for about 850 krn (ZalishshaL ad oh
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Stanovoy Metallogenic Belt of Grani
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Goryachev, 1995, 1998, 2003) consis
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Altinskoe, Aragochan, Dalnee, Dokhs
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comprises up to 70-80% in some ore
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The Au quartz vein deposits are int
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leucogranite plutons form large, ho
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+ , . Diorite phyry dike (Early ~ta
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- . --- Origin of and Tectonic Cont
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Britannia Metallogenic Belt of Kuro
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Specific Events for Late Early Cret
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Figure 73. Solnechnae Sin qu- ~d~ n
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- Origin of and Tectonic Controls f
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Nome Metallogenic Belt of Au Quartz
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quartz vein deposits of the Souther
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Selwyn Plutonjc Suite. The host roc
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along the western end in the Eagle
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101 Ma (K.M. Dawson, unpublished da
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I Bayonne Metallogenic Belt of Porp
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., (VV) belts. These zones and beb
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I (2) The East Sikhote-Alin (es) co
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Metallogenic Belt Formed in Late Me
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The Pb-Zn polyrnetallu: vein depb a
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olistolith. The deposit is currentl
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the core of the veins, chlorite, Mn
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Tayozhnoe Ag Epithermal Vein Deposi
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Figure 90. lskra deposit Sn polyrne
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- El (Late ~re&ceous) I+ we cmm=s)
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Figure 93. Mnogovershinnoe AMq @pWw
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immed by wehrlite, olivine-magnetit
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Eastern Asia-Arctic Metallogenic Be
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which would be hosted in the early
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Etandzha Porphyry Cu-Mo and Muromet
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0- / Fadt . . Au veins and pods Fig
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Sentachan Clastic-Sediment-Hosted A
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I I I Undifferentiated vdcanic and
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.r . : . -d ' . . ,, $44 . assembla
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closure, the Chukotka supertca&c wa
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- Mgh anglefau#or prsminant Fitwar
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intrude and crosscut both the relat
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Figure 101 8. Ke~ecolt &4W d KemwaI
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Figure 103. Generalized map of majo
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metallogenic belt (SP) which contai
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Eastern Asia-Arctic Metallogenic Be
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Valunistoe Au-Ag Epithermal Vein De
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Lost River Sn-W Skarn and Sn Greise
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Wheeler Creek, Clear Creek, and Zan
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Au veln,and hots spring deposits at
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Chicken Mountain Cu-Au Deposit The
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Chip sample location - Fault / Cont
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A proximate laatbm c#f C h # d ~nar
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0.03 1% Mo; and (3) for a hypogene
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others, 1994c. 1997~). The granitoi
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Cross section - - South greisen zon
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198 1). The mine at the deposit pro
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Beatson (Latouche) and Ellamar Bess
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CRETACEOUS Mount Leonard St& gueYtr
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n pJ pRanens. Pd-dc i3 Meeomic .---
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Figure 120. Huckleberry porphyry Cu
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0.15% Cu (ox), 0.127 g/t Au, and 0.
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Zone are 188 million tonnes grading
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Kitsault (B.C. Moly) Porphyry Mo De
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million tonnes grading 0.42% Cu, 0.
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extension. The Coryell Suite is int
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elated deposits. Forming in the bac
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Metallogenic Belts Formed in Tertia
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Hg Deposits Hg deposits occur throu
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Maletoivayam Sulfur-Sulfide Deposit
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(5) A major orthogonal junction for
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Metallogenic Belts Formed in Tertia
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occur in these tabular, altered sil
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summarlzed above are used by analog
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the Aleutian volcanic belt. The Yak
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metamorphism, anatectic granites, a
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References Cited Abbott, G., 1981,
Page 330 and 331: Society of America Abstracts with P
Page 332 and 333: Sciences, North-Eastern lnterdiscip
Page 334 and 335: Burgoyne, A.A., 1986, geology and e
Page 336 and 337: Canadian Cordillera, Yukon-northeas
Page 338 and 339: the Koryak Highlands: Transactions
Page 340 and 341: during 1984: U.S. Geological Survey
Page 342 and 343: Northeast Scientific Intergrated Re
Page 344 and 345: House, G.D., and Ainsworth, B., 199
Page 346 and 347: International Field Conference in V
Page 348 and 349: lithosphere in flood basalt genesis
Page 350 and 351: MacKevett, E.M., Jr., 1978, Geologi
Page 352 and 353: Miller, M.L., Bundtzen, T.K., and K
Page 354 and 355: Nekrasov, I.Ya., 1995, Genetic type
Page 357 and 358: Pakhomova, V.. Silyanik, V., Popov,
Page 359 and 360: Pollack, John, 1997, Summary report
Page 361 and 362: 1993: British Columbia Geological S
Page 363 and 364: Schroeter, T.G., 1987, Golden Bear
Page 365 and 366: Geology of the Liese zone, Pogo pro
Page 367 and 368: Colorado, Geological Society of Ame
Page 369 and 370: lnstitute of Mining and Metallurgy
Page 371 and 372: Anorthosite apatite-Ti-Fe Gabbroic
Page 373 and 374: TABLE 2. Summary of correlations an
Page 375 and 376: TABLE 2. Summary of correlations an
Page 377 and 378: 9! TABLE ectonic environment of Pro
Page 379: (Abbreviation) Rassokha (RA) Dzhard
Page 383 and 384: Major Mineral Deposits Types. Envir
Page 385 and 386: (Abbreviation) Guichon (GU) I Belt
Page 387 and 388: Major Mineral Deposits Types. Envir
Page 389 and 390: (Abbreviation) (Significant Mineral
Page 391 and 392: (Abbreviation) Adycha-Taryn (EAAT)
Page 393 and 394: ~etallo~enic Belt Major Mineral Dep
Page 395 and 396: Metallogenic Belt (Abbreviation) Ca
Page 397 and 398: TABLE 4. Significant lode deposits,
Page 399 and 400: Mineral Deposit Model Major Metals
Page 401 and 402: Deposit Name Mineral Deposit Model
Page 411 and 412: Deposit Nmme Mineral Deposit Model
Page 419 and 420: p;. ;A'..* Deposit Name Mineral Dep
Page 425: De~osit Name Mineral Deposit Model
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