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

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0 --mmm=oRuwrrrur ommmmarUaAll NEr- mmIL =-- DSII--llkr 6A-(ir 0 L . m m- On-- QI-amdm m--lkr M - m East, northern Japan, and adjacent offshore areas. Refer to text for descrip* t ,.si of metallogenic . ;-. belts. Adaeted from Nokleberq an others (1 997b, 1998) . < -.-- (6) In the same region is the aillespic (GE) metallogenic belt of SEDm Pb-Zn deposits that is hosted in the North American Craton Margin and is interpreted as forming during Intrusion of gabbro and diorite sills during Paleoproterozoic rifting. (7) In the same region is the Rapitan (RA) metallogenic belt of iron formation deposits that is hosted in the North hnerican Craton Margin. ##, This bell is interpreted as forming during marine exhalation along Mesoproterozoic North American Craton Margin. (8) In the P1 same region is the Redstone (RD) metallogenic belt of sediment-hosted Cu-Ag. deposits that is hosted in the North American Craton . . ~ar~in.-~his belt is interpreted as formingduring incipient Nwproterozoic rifting of the North American Cram Margin. (9) In the southern Canadian Cordillera is the Monashee (RD) metallogenic belt of SEDEX Zn-PbAg depmls. This belt, that is hosted in the Monashee terrane, is interpreted as a fiagment of North American Craton and formed during Late Proterozoic rifting of North American Craton. (10) In the same region, the Purcell (PR) belt of massive sulfide deposits is hosted in the North ~rnehcan Craton Margin, and is interpreted as forming during incipient rifting of the craton. And (1 1) in the same region, the Clark Range (CR) belt of sediment-hosted Cu-Ag deposits is hosted in the North American Craton Margin, and is interpreted as forming d&ng incipient rifling of the craton margin. In the below descriptions of metallogenic belts, only notable examples of significant lode deposits are described for each belt. Table 4, which is adapted and revised from Nokleberg and others (1997a), lists the significant lode deposits in each metallogenic belt. . ", .
EXPLANATION ORATOr( DMh&dy oceavaie roc*% AGhgquchem; ACN-; WAha: Nscm~Crrrn ltae Aaan C ~ W- -oy I NorthAsi&-tCrolonlUergR (VsrhhOya~'& kid ard UUUSI belt) block ARG Arpbs; BD 6adzhah D8 Debin; EK Ekonay; GB G-a; GL Galam; Cn Hldaka; IN Ind~g~rka: KK Karnuilrotan: KYB K m ; MU Mun~Ycan: NAB Nabitsky; NS NoraSukMh PA PemhinaAnadyr. F'K Pekubwy; SA Soulh Anyui: SMA Sarnarlur: CRATWTERRAMS TD Tukwingre-Wmgdi: TO Tokoro; TU T d ; UY Uyandb; AK Avdrm: AU Arg*r: BL Wadek: VE V w , YT Ve(lovskiy ~ ~ C X 0 ~ : O Y ~ l o n Dominenlly fiuW&es.' AMArrYSRVWAV- mSSNE CMCFTNWTAL- TERRAWES KUK Kur-lka: pwpd-RA-; AA Axttc Alaska: AY Aymsk; CH Chukotka; SY So~lchi-Y-, KN W-Nera: 00 W: QV hulevka: TL T a W i UL Ulban; 4 P-S: VL M I WK West Kamcba(ka METAMO- UMTWNTALdMRGIN TERRANES - ACCM~EDTERRANES PAC Pacilic oceanic plate mntakmam erc hmm Contad Actwe subduction zone ,ta,logmic - AAAh m m 0s' ALAlareyP: R m y : KM Karwrgd: -~MI(IIII*mKYKoyuRuk: U) bd+Grodekorsk; M4I m v . ME Elanws: NU Nulesyn: OKA Oiyulorks- Kanchafka: OL Oby: 98 SWbovskay; 3H Shrn~dt: TR -: HR MI PektAey: YA Y- Metallogenic Belts Formed During Proterozoic Rifting of North Asian Craton or Craton Margin Oroek Metallogenic Belt of ironstone and Sediment-Hosted Cu Deposits (Belt OK) West-Central Part of Russian Northeast BE Beryozovka: LN Len: SY SorrcM-Ye~o; UB Uniya-Bm: WSA W WhM: ZT Zhuravlesk-Tunnh The Oroek metallogenic belt of ironstone and sediment-hosted Cu deposits (fig. 2; tables 3,4)occurs mainly in the Shamaulikha River basin in the central part of tbe Russian Northeast (Shpikerman, 1998). The belt is hosted in the Shamanikha subterrane of the Prikdyma passive continental margin terrane of the Kolyma-Omolon superterrane (Noklebag d others, 1994c, 1997~). The belt trends north-south for 400 km along the axis of the Prikolyma terrane and has a maximum width of 100 km. The ironsione deposits occur in the Late Proterozoic Spiridon and Gorbunov Formations. The significant deposits are at P&eda and Oroek (Nokleberg and others 1997a, b, 1998). The Oroek metallogenic belt is herein interpreted as a faulted fragment of the Bilyakchan metallogenic belt, described below, which is hosted in the North Asian Craton Margin (Verkhoyansk fold belt, unit NSV). Pobeda Ironstone Deposlt One part of the Pobeda ironstone deposit (fig. 4) occurs in the Spiridon Formation consists of stratiform hematite (Z.G. Potapova, written commun., 1954; A.G. Kats, written commun., 1979) and is interpreted as a fossil littoral zircon-titanium- magnetite placer deposit. The other part of the deposit occurs in Late Proterozoic dolomitic marble of the Gorbunov Formation in a zone of imbricated thrust faults. This part of the deposit consists of gabbro and gabbro-amphibolite bodies and with hematite masses which occur along thrust fault planes. The deposit contains massive, brecciated, and stockwork ores. Massive ores contain
Page 1 and 2: I EUSGS science Ior a changing wwld
Page 3 and 4: CONTENTS Abstract .................
Page 5 and 6: 5 : 3 . Kedon metall lo genic Belt
Page 7 and 8: Parson and Brisco Barite Vein and G
Page 9 and 10: Overview ..........................
Page 11 and 12: Chepak Granitoid-Related Au Deposit
Page 13 and 14: Origin of and Tectonic Controls for
Page 17 and 18: Au-Ag Epithermal Vein Deposits Asso
Page 19: Metallogenesis and Tectonics of the
Page 22 and 23: and Byalobzhesky (1996). A volume c
Page 24 and 25: 1,079 significant mineral deposits
Page 26 and 27: Acknowledgements We thank the many
Page 30 and 31: Figure 3. Generalized map of mtljor
Page 32 and 33: Archean granulite facies metamorphi
Page 34 and 35: Figure 5. Oroek sediment-h section
Page 36 and 37: 1 a a - --rich sandstone ~b-Qmg@ner
Page 38 and 39: Origin of and Tectonic Setting for
Page 40 and 41: occur in clastic and impure carbona
Page 42 and 43: Figure 7. Sullivan sedimentary-exha
Page 44 and 45: I 1997a, b, 1998). The massive sulf
Page 46 and 47: Ma which locally form extensive plu
Page 48 and 49: Figure 10. Gerbikanskoe vdcanogenic
Page 52 and 53: from crystalline basement of craton
Page 54 and 55: Figure 13. Howards Pass sedknenWy e
Page 56 and 57: McLean Arm Porphyry Cu-Mo District
Page 58 and 59: [..'......I Surfia'al deposits (Hol
Page 60 and 61: Figwe 16. GeneraCied map of major M
Page 62 and 63: .- *.-* *. . - - ---- -A - EARLY MI
Page 64 and 65: Metallogenic Belt Formed During Col
Page 68 and 69: several tens of meters to 1,300 m l
Page 70 and 71: Goldfarb (197) who interprets that
Page 72 and 73: WTF and Red Mountain Kuroko Massive
Page 74 and 75: interpreted by and as part of a ext
Page 76 and 77: Mount Sicker Metallogenic Belt of K
Page 78 and 79:
interpreted as vents. The deposit c
Page 80 and 81:
Origin of and Tectonic Controls for
Page 82 and 83:
Page 84 and 85:
Page 86 and 87:
hosted in the Yarkhodon subterrane
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origin of the younger Triassic(?) B
Page 90 and 91:
Page 92 and 93:
Mississippian age of mineralizalioi
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Monger and Nokleberg, 1996; Noklebe
Page 96 and 97:
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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Page 108 and 109:
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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Page 134 and 135:
Figure 46. Lawyers Au-Ag epitiefmel
Page 136 and 137:
Page 138 and 139:
(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
Page 146 and 147:
Page 148 and 149:
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
Page 156 and 157:
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
Page 164 and 165:
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
Page 192 and 193:
Britannia Metallogenic Belt of Kuro
Page 194 and 195:
Specific Events for Late Early Cret
Page 196 and 197:
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
Page 202 and 203:
quartz vein deposits of the Souther
Page 204 and 205:
Selwyn Plutonjc Suite. The host roc
Page 206 and 207:
along the western end in the Eagle
Page 208 and 209:
101 Ma (K.M. Dawson, unpublished da
Page 210 and 211:
I Bayonne Metallogenic Belt of Porp
Page 212 and 213:
., (VV) belts. These zones and beb
Page 214 and 215:
I (2) The East Sikhote-Alin (es) co
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Metallogenic Belt Formed in Late Me
Page 218 and 219:
The Pb-Zn polyrnetallu: vein depb a
Page 220 and 221:
olistolith. The deposit is currentl
Page 222 and 223:
the core of the veins, chlorite, Mn
Page 224 and 225:
Tayozhnoe Ag Epithermal Vein Deposi
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Figure 90. lskra deposit Sn polyrne
Page 228 and 229:
- El (Late ~re&ceous) I+ we cmm=s)
Page 230 and 231:
Figure 93. Mnogovershinnoe AMq @pWw
Page 232 and 233:
immed by wehrlite, olivine-magnetit
Page 234 and 235:
Eastern Asia-Arctic Metallogenic Be
Page 236 and 237:
which would be hosted in the early
Page 238 and 239:
Etandzha Porphyry Cu-Mo and Muromet
Page 240 and 241:
0- / Fadt . . Au veins and pods Fig
Page 242 and 243:
Sentachan Clastic-Sediment-Hosted A
Page 244 and 245:
I I I Undifferentiated vdcanic and
Page 246 and 247:
.r . : . -d ' . . ,, $44 . assembla
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closure, the Chukotka supertca&c wa
Page 250 and 251:
- Mgh anglefau#or prsminant Fitwar
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intrude and crosscut both the relat
Page 254 and 255:
Figure 101 8. Ke~ecolt &4W d KemwaI
Page 256 and 257:
Figure 103. Generalized map of majo
Page 258 and 259:
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
Page 268 and 269:
Au veln,and hots spring deposits at
Page 270 and 271:
Chicken Mountain Cu-Au Deposit The
Page 272 and 273:
Chip sample location - Fault / Cont
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A proximate laatbm c#f C h # d ~nar
Page 276 and 277:
0.03 1% Mo; and (3) for a hypogene
Page 278 and 279:
others, 1994c. 1997~). The granitoi
Page 280 and 281:
Cross section - - South greisen zon
Page 282 and 283:
Page 284 and 285:
198 1). The mine at the deposit pro
Page 286 and 287:
Beatson (Latouche) and Ellamar Bess
Page 288 and 289:
Page 290 and 291:
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
Page 306 and 307:
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
Page 314 and 315:
Page 316 and 317:
(5) A major orthogonal junction for
Page 318 and 319:
Metallogenic Belts Formed in Tertia
Page 320 and 321:
occur in these tabular, altered sil
Page 322 and 323:
summarlzed above are used by analog
Page 324 and 325:
the Aleutian volcanic belt. The Yak
Page 326 and 327:
metamorphism, anatectic granites, a
Page 328 and 329:
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
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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
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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
Page 387 and 388:
Major Mineral Deposits Types. Envir
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(Abbreviation) (Significant Mineral
Page 391 and 392:
(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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