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

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Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Central Kamchatka Metallogenic Belt of Au-Ag Epithermal and Porphyry Cu-Mo Deposits (middle and late Tertiary) Kamchatka Peninsula (Belt CK) Aginskoe (Aga) Au-Ag epithermal vein Au, Ag, Te 55'31'N 15752~ Baran'evskoe Chernpura Au-Ag epithermal vein Volcanic-hosted Hg Au. Ag Hg 55'06'N 56' 1 2W 158'1 3'E 1 59' I WE Krasnogorskoe Porphyry Cu-Mo Mo 53'58~ 1 57m28'~ Oganchinskoe Ozernovskoe Au-Ag epithermal vein Au-Ag epithmal vein Au. Ag Au. Ag, Te 54'57~ 1 57.46'~ 57-35 w 1 60~47'~ Sukharikovskie Grebni Au-Ag epithermal vein Au, Ag 55.40~ 158'39'~ Tutkhlivayam Au-Ag epihennal vein Au, Ag. Cu, Pb, Zn, Te, Cd 59'04~ 161'44'~ Zolotoi Au-Ag epithennal vein Au, Ag 55'03W 158.211E Alaska Peninsula and Aleutian Islaads Metallogenic Belt of lgneoos Arc Deposits (middle Tertiary) WesternSouthern Alaska (Belt AP) Apollo-Sitka Au-Ag epithemal vein AU, ~ g Pb, , Zn, Cu 55.12~ 160'3r~ Aquila Au-Ag epithermal vein Au, Ag 55'1 1% 160~420'~ Bee Creek Porphyry Cu Cu, Au 56-31W 158'24'~ Canoe Bay Au-Ag epithermal vein Au. Ag 55.35~ 161'16'~ Cathedral Creek, Braided Creek Polyrnetallic vein Cu, As, Zn. Pb 56*33(YN 158-44'~ Fog Lake (Pond) Au-Ag epirhennal vein Au, Cu, Ag 59'31W 154'23~ Kawisgag (Ivanof) Porphyry Cu md (or) potymetallic vein Cu, Mo, Au 55'57~ 1 59'24'~ Kilokak Creek Polymetallic vein(?) Pb, Zn 57'1 1 'N 156.24'~ KUY Au-Ag epithermal vein Au, Ag, Cu 59.16~ 154'38'~ Mallard Duck Bay Porphyry Cu-Mo and(or) polymetallic vein(?) Cu, Mo 56'14% 158.30'~ Mike Porphyry Mo Mo 57.03~ 157'13'~ Pyramid Porphyry Cu Cu, Au 55'37% 160~41'~ Rex San Diego Bay Porphyry Cu Au-Ag epithcrmal vein(?) Cu, Au Ag, Au, Cu. Pb, Zn 5f 1 2 ~ 157'00'~ 55.34~ 16027'~ Sedanka (Biorka) Polymetallic vein Zn, Pb, Cu 53'451~ 166'1 O'W Shurnagin Au-Ag epithermal vein Au. Ag 5g12~ 1 60.35'~ Warner Bay (Prospect Bay) Porphyry Cu, Polymetallic vein Cu, Mo, Pb. Zn 56'1 OW 158-220'~ LATE TERTIARY and QUATERNARY (Pliocene through Present - 4 to 0 Ma) Sakhalin Island Belt of Silica-Carbonate and Volcanic-Hosted Hg Deposits (late Tertiary) In' River Kuril Islands, Sakhalin Island, Russian Far East (Belt SH) Volcanic-hosted Hg wl Hg, Cu 50'33~ 142'32'~ lnskoe Ostrinskoe Svetlovskoe Volcanic-hosted Hg Silica-carbonate Hg Silica-carbonate Hg HI3 Hg Hg 48.52~ 142'38% 49'44% 143'1 2'~ 50'09~ 143'23% Yasnoe Silica-carbonate Hg Hg 50~338~ 142.2~~ Kuril Metallogenic Belt of Au-Ag Epithermal Vein, Cu-Pb-Zn Polymetallie Vein, Sn silica-sulfide vein, Sn Vein, Sulfur-sulfide (Volcanic S), Kuroko Massive Sulfide, and Porphyry Mo Deposits (middle Tertiary to Holocene) Kuril Islands, East-Central Part of Russian Far East (Belt KU) Carpinsky Caldera Porphyry Mo Mo 50'10'~ 155'28'~ Dushnoe Cu-Pb-Zn polymetallic vein Cu. Zn, Pb 4658~ 152'04'~ Ebeko Sulfur-sulfide s, F 6 50'38~ 156'03~ Golovninskoe Sulfur-sulfide. S, FeS 43-53W 145'36'~ Koshkina Polyrnetallic vein Cu, Zn. Pb 50.44~ 15d16'E Krishtofovich Volcano Sulfur-sulfide S, FeS2 45'47~ 149~43'~ Novoe Sulfur-sulfide S, FeS2 44-56~ 147'30'~ Prasolovskoe Au-Ag epithemal vein. Au, Ag 44'1 9 ' ~ 146'05% Reidovskoe Porphyry Mo Mo 45'1 2'N 148'1 2% Ri fovoe Au-Pb-Zn epithermal vein Au, Zn, Pb 5d24'~ 1 56'02'~ Rudnikovskoe Sn silicate-sulfide vein Sn, Pb, Zn 44'37'N 147.22'~ Sernaya River Au epithermal vein Au, Zn, Cu 45'1 0% 148'02'~ Sofya Spiridonovskoe Au epithermal vein Sn polyrnetallic vein Au Sn. Pb, Zn 45'27'~ 14~~43'~ 44'0 1 W 145'45'E Tet'yaevskoe Cu-Pb-Zn polymetallic vein Cu, Zn, Pb 45b1'~ 149'35'E 405
De~osit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Valentinovskoe Vysokoe Zaozernoe Kuroko Cu-'Pb-Zn massive sulfide Cu, Pb, Zn 44* 12'~ 145~58'~ Sulfur-sulfide S, FeSl 45"0 1 'N 147'54'~ Sulfur-sulfide S, FeS2 50~30'~ 1 56'02'~
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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
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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 423: Deposit Name Mineral Deposit Model
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