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

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Talarninskoe Tokur Sb-Au vein Au quartz vein Sb, Au 5222'~ 133'24% Au 53'09~ 1 32'49% Bamskoe (Chul'baneo) " / Burindinskoe Northern Part of the Russian Southeast (Belt ST) Au-AE e~ith~rmal vein Au . Ae - AU-A; epithd vein Au, Ag 55*59U 123'54% 53'4 I 'N 124'54'~ Kirovskoe Granitoid-releted Au 54.27~ 124.14'~ Kular Metallogenic Metallogenic Belt of Au Quartz Vein, Cranitoid-Related Au, Au-REE Quartz Vein, and Sn Quartz Vein Deposits (Early Cretaceous), Northern Part of Eastern Siberia (Belt KU) Burguat Au quartz vein 70'42~ 134.3 18 Dzhuotuk 70'1 3~ 1 34'1 7% Novoe 69.36'~ l33*07% Solur 70'01'~ 133'24% Bular Burgali Dies Allakh-Yun Metdoplrmk Belt of Au Quartz Vein Deposits and Associated W-Sn Quartz Vein Deposits Au quartz vein Au 6lW13'N 137'50'E Porphyry-MO 0 Mo, W 59.56~ 138'5 1 'E Cu skam Cu 59'10~ 138'1 I'E Duet Au quartz vein Au 59'48~ 137'44% It-Yuryak W vein, Sn oqm& vein W Levo-Dybin Granitoid-related Au An, W, Bi Malyutka Au quartz vein Au Muromets Cu-Mo skam Cu, Mo, W Nezhdaninka Au quartz vein Au, Ag Novinka Au quartz vein Au Onello (Lider) Au quartz vein Au Svetly Voskhod Yur Au quartz vein AU ; 3 Y l Au quartz vein Au 61'221~ 139.22% Au quartz vein AU Zaderzhnoe Au quartz vein Au Zhar Au quartz vein Au Yana-Polousnen Metallogenic Metallogenic Belf of Granitoid-Related Sn Quartz Vein, W and ~n-~karn. ~n-silicate Sulfide Vein and Related Dewsits Early Cretaceous), Central Part of Russian Northeast (Belt YP) Altinskoe Polymedic vein Pb, Zn 69'47'~ 142' 14'~ Alys-Khaya SR polymetallic vein Sn 65'56~ 135'43'~ Anornalnoe Aragoc han Arbatskoe Argin Sn silicate-sulfide vein Polymctallic vein Co &am Sn quartz vein Sn Pb, Zn Co Sn 65'37~ 13 1'493 69.44~ 137'00% 69'28~ 149'418 1 - , 68.03~ 135'5O'E 1 Balyktaah, Ploskoe Bugdogar Burgachan Chistoe Dalnee Dokhsun Ege-Khaya Il~n-Tas Sn pisen Sn polymehllic vein Sn polymetallic vein Granitoid-related Au Polymetallic vein Polyrmstallic vein Sn polymettllic vein Sn silicsre-sulfide vein Sn Sn Sn AU Pb, Zn Pb, Zn, cu Sn. Zn Sn 69.50~ 1 5 1'488 65'12'~ 133'59'~ rq 65.46~ 134-45'~ i: 69'43'N 150'151 [1 69'49~ 138.308 69'26N 144.2~~ IP 6738~ 134'478 65'6~ 135'56'~ Kandidatskoe Kester Au skam Sn greism Au. CO, As Sn, Ta, Nb, Li 69.24~ 149~44'~ 6f17'N 134.38'~ Khoton-Khava Sn-polymctallic . - vein, Sn silicate-sulfide vein Sn 67'17'N 133'47% Pol yarnoe Sn greisen and vein Takalkan Sn greisen Tuguchak- l Mo quartz vein Tuguchak-2 Granitoid-related Au " -- 9
Deposit Name Mineral Deposit Model Major Metals Latitude N; Longitude E, W. Ulakhan-Egelyakh Sn silicate-sulfide vein Sn 67'09'~ 134-2 1 'E Ulakhan-Sala Sn silicate-sulfide vein Sn 69'48'~ 136'40'~ Verkhne-Naanchan Polymetallic vein Pb, Zn 69'39'~ 1 50-4 1 'E Darpir Metallogenic Belt of Sn and Associated Felsic-Magmatism Deposits (Early Cretaceous) Western Part of Russian Northeast (Belt DP) Bastion Sn greisen Sn 63'17'~ 153"13'E Bolshoy Kanyon Sn skarn Sn 63" 15'~ 1 5 1-05'~ Chepak Granitoid-related Au Au, W, Bi 63O05'N 152"45'E Chibagalakh Sn-B skam B, Sn 68"13'N 139"5 I'E Darpir Sn silicate-sulfide vein Sn 64'02~ 147~42'~ Lazo Sn silicate-sulfide vein Sn 63-1 2'N 1 52'1 3'E Titovskoe Sn (B) magnesian skarn B 67"33'N 139'14'~ Verkhne-Seimchan Co-As vein Co, Bi 63-1 7% 15 1"23'E Tompon Metallogenic Metallogenic Belt of Cu, W, Sn Skarn, and Sn Quartz Vein Deposits (Early Cretaceous) West-Central Part of Eastern Siberia (Belt TO) Agylki W skarn W, Cu 64"17'N 137~16'~ Erikag Sn quartz vein Sn 64'30'~ 137-1 8 ' ~ ~hunkhada W-Sn skarn W, Sn 64'34'~ 134"49'E Shamanikha Metallogenic Belt of Au Quartz Vein and Cu-Ag Quartz Vein Deposits (Late Jurassic to Early Cretaceous) Central Part of the ~ussian Northeast ( ~elt SH) Glukhariny Au quartz vein Au 64*58'N 153~04'~ Kopach Au quartz vein Au 65'2 1 'N 1 52'57'~ OPY t Cu-Ag quartz vein? Cu, Au, Pb, Zn, Ag, Au 63O54'N 152'33'~ Verkhoyansk Metallogenic Belt of Au Quartz Vein, Au-Sn Polymetallic Vein Deposits (Late Jurassic and Early Cretaceous), Western Part of Russian Northeast (Belt VK) Anna-Emeskhin Au quartz vein Au 68O56'N 128'24'~ Balbuk Pb polymetallic vein Pb 64'49'~ 130'37'~ Bochiyskoe Sn polymetallic vein Sn 66'14'~ 1 29'58'~ Chochimbal Polymetallic vein Au, Ag, Pb 65"54'N 129'45'~ Dyabkhanya Au polymetallic vein Au, Ag 65'30'~ 129'60'~ Enichan-Tolono Au quartz veln Au 68-1 I'N 128'1 I'E Galochka Au quartz vein Au 65*42'N 128'26'~ Imtandzha Sn polymetallic vein Sn 66'08~ 1 29'36'~ Nikolaevskoe, Otkrytoe Au quartz vein Au 70'20'~ 129'33'~ Syncha-I & 11 Au quartz vein Au 67'50~ 128'03'~ Syugyunya kh-Kende Au quartz vein Au 68-42'N 127-46'~ Yana-Kolyma Metallogenic Belt of Au Quartz Vein, So Vein and Greisen, W Vein and Clastic-Sediment-Hosted Hg Deposits (Late Jurassic and Early Cretaceous), Central Part of Russian Northeast (Belt YA) Aleshkino Au quartz vein Au 67'1 I'N 138'22'~ Alyaskitovoe Sn-W greisen Sn, W 64'48~ 141'52'~ Badran Au quartz vein Au 64'12~ 141*411E Baryllyelakh Sn greisen Sn, W 63"35'N 143"54'E Bazovs koe Au quartz vein Au 6422'~ 14 1'26'~ Bekkem W-Mo-Sn vein and greisen W 64'04~ 142-37'~ Bokhapcha W vein and greisen W 6 1'45'~ 150b4'~ Burgavli Sn quartz vein Sn 66'28'~ 1 37-39'~ Burkat Sn quartz vein Sn 65'35~ 1 40~59'~ Burkhala Au quartz vein Au 62'36'~ 149~04'~ Butugychag Sn quartz vein Sn 61-1 5'N 149-05'~ Chai-Yurya Au quartz vein Au 62'4 1 'N 147'24'~ Chelbanya Au quartz vein Au 62'37~ 148'02'~ Daika Novaya Au quartz vein Au 62'45~ 148'06'~ Darpir Au quartz vein Au 65'30~ 138'55'~ Degdekan Au quartz vein Au 6 1-58'~ 146~60'~ Delyuvialnoe Granitoid-related Au Au 66-1 7'N 1 36"53'~ Dirin-Yuryak Au quartz vein Au 64"25'N 142"19'E Djelgala-Tyellakh Au quartz vein Au 62'1 9'N 148"501E Dorozhnoe Au quartz vein Au 62'50'~ 148~02'~ Ekspeditsionnoe Au quartz vein Au 61~41'~ 150"33'E
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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
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 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 407: 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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