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

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Gambier Metallogenic Belt of Porphyry Cu-Mo and Zn-Pb-Cu Skarn Deposits (early Tertiary) Southern British Columbia @It GB) Garnbier Island (092GNW 025) Hi-Mars (~ewis '~ake) (092F 292) Pomhvrv . .. Cu-Mu Porphyry Cu-Mo Cu, Mo Cu, Mo 49'3 1 15 1 23.22~ 49'57'~ 124.2 1 w Lynn Creek (092GSW 003) O.K. (092K 008; 092K 057) Zn-Pb ekam Porphyry Cu-Mo Zn, Pb Cu, MO 49'25~ 123'04W 00 1) Bell Moly (Alice Arm) ( 1 03P 234) Porphyry Mo Mo, W Berg (093E 046) Parphyry Cu-Mo Big Onion (093L 124) Porphyry Cu-MO Capoose Lake (093F 040) &Au potymetallic vein Dorothy (093M 009) Porphyry Cu-Mo Equity Silver (Sam Goosly) (093L 001) Ag potymetallic vem Granisle (093L 146) Porphyry Cu-Au (Mo) Cu, Au, Ag 54.57W 126*09'V&~ Kitsault (BC Moly) (I 03P 120) Porphyry Mo Mo 55.25~ 129'25'wF Lucky Ship (093L 053) Porphyry Mo Mo 54.02~ 126'59~ Morrison Porphyry Cu-Au (Mo) 55'1 I'N 126'19'~ Mount Thomlinson (093M 080) Pvrphyry Mo Mo Nanika (DW, New Nanik) (093E Porphm Cu-Mo Cu 055) Prosperity-Porter Idaho (103P Ag-Pb-Zn polyrnetellic mh Ag, Pb, Zn 089) Highland Bell (Beaverdell) (O82ESW 030) Lassie Lake Area (Blizzard) Palmplacer U (082ENE 046) Millie Mack (082KSW 057) Au-Ag polymetdlic vein Bluebell (Riondel) (082ENE 42, Zn-Pb-Ag sksm and manto 403
Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Kvinumsky Metallogenic Belt of Hornblende Peridotite and Gabbroic Ni-Cu Deposits (early Tertiary) Russian Southeast (Belt KV) Kuvalorog Hornblende peridotite Cu-Ni. Cu, Ni 53'28'~ 157"24'E Kvinum Gabbroic Cu-Ni Ni, Cu, Co, Au, Pt 53-38'~ 157'02'~ Shanuch Hornblende peridotite Cu-Ni. Ni, Cu, Co, Au, Pt 55'09'~ 157'12'~ Central Koryak Metallogenic Belt of Igneous Arc Deposits (Late Cretaceous and early Tertiary) East-Central Part of Russian Northeast (Belt CKY) Agranai Volcanic-hosted Hg Hg 6333~ 173'1 O'E Ainatvetkin Ametistovoe Berezovaya Ivolga Sn polymetallic vein Au-Ag epithermal vein Sn polymetallic vein Epithermal vein Sn, Ag Au, Ag Sn Ag, Sn 60-58'~ 1 65'1 7'E 6lS19'N 164~49'~ 63"60'N 173-52'~ 61'16'~ 165"211E Mi;: f%l , Khrustal (Khrustalnoe) Sn polymetallic vein Sn 6 1°28W 167-1 O'E Krassnaya Gorka Clastic sediment-hosted Hg or hot-spring Hg? Hg 6 1'54'~ 1 68"48'E Kuibiveen Porphyry Cu-Mo Mo, Cu, Au 62'43~ 1 70"06'E Lalankytap Porphyry Cu-Mo Mo, Cu 62'09~ 173~1 1 'E Larnut Volcanic-hosted Hg Hg 64"05'N 172~60'~ Lyapganai Clastic sediment-hosted Hg or hot-spring Hg? Hg, Sb 61'34~ 168'0 1 'E Neptun Clastic sediment-hosted Hg or hot-spring Hg? Hg, Sb, As 6 1'40'~ 168-1 6'E Orlovka Epithermal vein Au, Zn, Cu, Hg 64'00'~ 168~34'~ Parkhonai Sn polymetallic vein and Sn silicate-sulfide vein Sn 64°04'~ 173'1 8% Pervenets Silica-carbonate Hg Hg, As, Sb 63"28'N 173'5 1 'E Reznikov Sn polymetallic vein Sn, Ag, Au 60-50'~ 1 64'39'~ Rzhavy Porphyry Cu-Mo Cu, Mo, Au 65'47'~ 165'06'~ Sprut Au-Ag epithermal vein Ag, Au 6 1'2 1 'N 1 65*07'E Tamvatney Silica-carbonate Hg Hg, W, As 63*29'N 174'1 3'E Unnei Sn polymetallic vein Sn, Ag, Au 6 1-3 1 'N 1 66-07'~ Olyutor Metallogenic Belt of Igneous-Arc-Related Deposits (late Paleogene, Miocene, and Pliocene) Kamchatka Peninsula (Belt OT) Maletoivayam Sulfur-sulfide S 60~26'~ 164"23'E Olyutor Clastic sediment-hosted Hg or hot-spring Hg? Hg, Sb, As 60~35'~ 167'49'~ Pinchi Lake Metallogenic Belt of Hg Epithermal Vein, Sb-Au Vein, Silica-Carbonate Hg Deposits (Oligocene and Miocene), Central British Columbia (Belt PC) Pinchi Lake Silica-carbonate Hg Hg 54'38~ 124"26'~ Owl Creek Metallogenic Belt of Porphyry Cu-Mo; Porphyry Mo and Au Polymetallic Vein Deposits (Oligocene and Miocene), Southern British Columbia (Belt OC) Clear Creek (Gem) (092HNW 001) Porphyry Mo Mo 49"43'N 12 l"43'~ Owl Creek district (092JSE 004, 006,007) Porphyry Cu-Mo Cu, Mo 50'23~ 122"45'W Salal Creek (092JW 005) Porphyry Mo Mo 50~46~ 123'24'~ MIDDLE TERTIARY (Miocene - 20 to 10 Ma) East Kamchatka Metallogenic Belt of Au-Ag Epithermal Deposits (Miocene) Central and Southern Kamchatka Peninsula (Belt EK) Asachinskoe Au-Ag epithermal vein Au, Ag, Se 52*08'N 157'54'~ Kitkhoi Au-Ag epithermal vein Au, Ag, Zn, Pb 53*26'~ 1 58'1 7'E Kurnroch Au-Ag epithermal vein Au, Ag, Cu, Pb, Zn 55'40~ 161'1 0'E Mumovskoe Au-Ag epithermal vein Au, Ag, Cu, Zn, Pb 52"44'N 158~24'~ Rodnikovoe Au-Ag epithermal vein Au, Ag 52O50'N 158'1 6 ' ~ .q::c
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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,
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Society of America Abstracts with P
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Sciences, North-Eastern lnterdiscip
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Burgoyne, A.A., 1986, geology and e
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Canadian Cordillera, Yukon-northeas
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the Koryak Highlands: Transactions
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during 1984: U.S. Geological Survey
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Northeast Scientific Intergrated Re
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House, G.D., and Ainsworth, B., 199
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International Field Conference in V
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lithosphere in flood basalt genesis
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MacKevett, E.M., Jr., 1978, Geologi
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Miller, M.L., Bundtzen, T.K., and K
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Nekrasov, I.Ya., 1995, Genetic type
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Pakhomova, V.. Silyanik, V., Popov,
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Pollack, John, 1997, Summary report
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1993: British Columbia Geological S
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Schroeter, T.G., 1987, Golden Bear
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Geology of the Liese zone, Pogo pro
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Colorado, Geological Society of Ame
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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 and 380: (Abbreviation) Rassokha (RA) Dzhard
Page 381 and 382: Metallogenic Belt (Abbreviation) Be
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 421: Deposit Name Mineral Deposit Model
Page 425: De~osit Name Mineral Deposit Model
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