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

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Figure 49 Generaltzed map Of mbjm Lab &as$& b * * ~ ~ ( b r ~ t . d * c m ~ m - ~ a - ~ ~ ofhhon m. b m Ibr dac- d -. khptd mkldmrg and ahrS(MWb, W). Ww l* 3 for explanation the Wrangellia island-arc supertem. 'I&k bdl is &*dd a h thp &&IU =-*.&* la the below descriptions of metallogsaio bdm, II hv d & a 6- kda (et%)m.M-M - .+- .,., bsh. . Metallogenic-Tectonic Model for Late Jurassic (163 to 144 Ma; Figur, !Bj hrbg the Latc Jarnssic (Oxfpr6r~ hhtoryb -; 1 E4 lo 1 4 e}, the were (fig. 50; table 3): ( 1 ) ~ a f ~ c r C ~ ~ ~ ~ h N fomtion of associated mstrllogak kk wqmb -rrrw amd arc re3d assachd tmme.9 edo Lbe Nost4-h hhn B+#!u$ @ (3) obductbw of tbe ~ L - ~ previous long-lid pcrmd (Late Pmteroeok hugb Early J d c ) ctfpoaaive sdmenMth on &c H&& A9ibsrdM American Cratons - - 4 I Specific Events Lslr J u m Forming in the arc wem the T--M (TAM) klt of podlfm CT whU ie bid haone plutons, and the AaaiRif3 (MI beh afhnroko massive suW depab. Tbtl- Ihbd to UIC wadaccretionary-wedge tmme (AV) *& h t d km ruWucLim ofpaff of- mxuic t ': subduction zone m m ~w~ toward the Kcmy-Mu@ iald art. (2) The Modin rn (Madin vvl~ic-pblonic MI, nM) hnb the U&km arc ( U m B m - m V-W& . belt, uo and associated units) coslinud acdvicy. F a in Ihp mc mr t& No& Bmym (MI) rnehlbgmk Wt, w&& wmtisw subduction-related ~ c - depouil$. m A s w~ W ~f~ ~ of& ares w& &tbtW@fw bf. . . I ? . ..
AR - Ariadny -- -- ---- -- - - - -. - - - - - - - - - -* - . . . . - . > . -- . - - ... ------.. ..-- -*- -..-- - --- . -- ---- - -. . . .- - - TM - TJkeelno Mountoim ESA - Eostem-Southem TO - foodoggrns Medro RL - R~sdond FM - F- ST - W IP - l dad Paphm SUN - S ~ - N O C KB-Kobuk SWA - Swlhweslem Alosko KL - K l - m YR . . . - Vukm . -. . -. . . R . . -. i KUY - Kuyul YS MA - - Yamzhaye River 163 to 144 Ma Figure 50. Late Jurassic (Oxfordian through Kimmeridigian - 163 to 144 Ma) stage of metallogenic-tectonic model. Refer to text for explanation of metallogenic-tectonic events, to tables 3 and 4 for descriptions metallogenic belts and significant deposits, and to figure 18 for explanation of abbreviations, symbols, and patterns. Adapted from Nokleberg and others (1997b, 1998, 2000). the Ancestral Pacific Ocean plate to continue forming the Samarka (SMA), Khabarovsk (KB), and Badzhal (BD) terranes. Forming along the transform continental margin was the Ariadny (AR) belt of zoned mafic-ultramafic Ti deposits which is hosted in zoned mafic-ultramafic plutons intruding the Sarnarka subduction-zone terrane. (3) In the same region, the Bureya (BU) superterrane accreted against the Ulban accretionary-wedge terrane (UL) along the Mongol-Okhotsk suture (MO) thereby closing the Mongol-Okhotsk Ocean. Forming during accretion was the Stanovoy (ST) metallogenic belt which contains anatectic, granitic-magmatism-related deposits. (4) The Uda continental-margin arc (Uda volcanic-plutonic belt, ud, and Uda-Zeya sedimentary basin, uz) continued to form. Associated with the arc was subduction and sinistral transpression of part of the Mongol-Okhotsk Ocean plate to form the Turkuringra-Dzhagdinsk (TD), and Ulban (UL) terranes. Subduction was associated with sinistral transpression along the Mongol-Okhotsk suture (MO). (5) The extensive Kony-Murgal continental-margin and island-arc terrane (KM) continued to form as an extension of the Uda continental-margin arc (ud). Associated with the arc was continued subduction of part of the ancestral Pacific Ocean plate to form the Talovskiy (TL) and Penzhina-Anadyr (PA) terranes. The Kony-Murgal island arc overlapped the Okhotsk (OK) and Avekova (PJO cratonal terranes which were previously rifted from the North Asian Craton (NSC), and the Viliga (VL) passive
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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
Page 90 and 91: Origin of and Tectonic Controls for
Page 92 and 93: Mississippian age of mineralizalioi
Page 94 and 95: Monger and Nokleberg, 1996; Noklebe
Page 96 and 97: 1997a, b). Most of the magnesite an
Page 98 and 99: FL - Finlayson Lakm FR-FmLake LI -
Page 100 and 101: disseminations in chert, disseminat
Page 102 and 103: U F~gure 32 GemMzed m p of mejw -ni
Page 104 and 105: terrane, and by the Stikine Assembl
Page 108 and 109: Metallogenic-Tectonic Model for Lat
Page 110 and 111: . I . r ; 4 ~ (9) During subduction
Page 112 and 113: Eastern Alaska Range Metallogenic B
Page 114 and 115: individual flows range from 5 cm to
Page 116 and 117: occurrence of turbiditic clastic ro
Page 118 and 119: along the with tectonically-related
Page 120 and 121: : m- 3- w43 k M- u m u~u) mtl 'M~!A
Page 122 and 123: island-arc volcanic rocks of the Ni
Page 124 and 125: -- - //// EpldoW Figure 41. Nickel
Page 126 and 127: (TC), and Toodoggone (TO) belts whi
Page 128 and 129: (4) The Angayucham Ocean (Kobuck Se
Page 130 and 131: lueschist units and the McHugh Comp
Page 134 and 135: Figure 46. Lawyers Au-Ag epitiefmel
Page 138 and 139: (5) The Angayucham Ocean (Kobuck Se
Page 142 and 143: continental-margin terranes which w
Page 144 and 145: Pokrovskoe Au-Ag Epithermal Vein De
Page 148 and 149: Granite-porphm and wanits W e ~~ hl
Page 150 and 151: subordinate adularia, dolomite, cel
Page 152 and 153: shale, basalt, plagiorhyolite, silt
Page 154 and 155: ocks and serpentinite which occur a
Page 156 and 157: interpreted as forming in the Juras
Page 158 and 159: Fault / Figure 57. Bond Creek and O
Page 160 and 161: Klukwan-Duke Metallogenic Bett of M
Page 162 and 163: tonnes of ore mined between 1967 an
Page 164 and 165: Cariboo Metallogenic Belt of Au Qua
Page 166 and 167: Sheep Creek Au-Ag Polymetallic Vein
Page 168 and 169: ---. .% of the North American Conti
Page 170 and 171: - OwiapaasembC Cmhmmmand Cemmcl. an
Page 172 and 173: in the west-central part of the Rus
Page 174 and 175: for about 850 krn (ZalishshaL ad oh
Page 176 and 177: Stanovoy Metallogenic Belt of Grani
Page 178 and 179: Goryachev, 1995, 1998, 2003) consis
Page 180 and 181: Altinskoe, Aragochan, Dalnee, Dokhs
Page 182 and 183: comprises up to 70-80% in some ore
Page 184 and 185: The Au quartz vein deposits are int
Page 186 and 187: leucogranite plutons form large, ho
Page 188 and 189: + , . 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
Page 352 and 353:
Miller, M.L., Bundtzen, T.K., and K
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Nekrasov, I.Ya., 1995, Genetic type
Page 357 and 358:
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
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TABLE 2. Summary of correlations an
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TABLE 2. Summary of correlations an
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9! TABLE ectonic environment of Pro
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(Abbreviation) Rassokha (RA) Dzhard
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Metallogenic Belt (Abbreviation) Be
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Major Mineral Deposits Types. Envir
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(Abbreviation) Guichon (GU) I Belt
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Major Mineral Deposits Types. Envir
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(Abbreviation) (Significant Mineral
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(Abbreviation) Adycha-Taryn (EAAT)
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~etallo~enic Belt Major Mineral Dep
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Metallogenic Belt (Abbreviation) Ca
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TABLE 4. Significant lode deposits,
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Mineral Deposit Model Major Metals
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Deposit Name Mineral Deposit Model
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Deposit Nmme Mineral Deposit Model
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p;. ;A'..* Deposit Name Mineral Dep
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De~osit Name Mineral Deposit Model
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