Columbia Department <strong>of</strong> Mines <strong>and</strong> Petroleum Resources, p. 93-97. Su<strong>the</strong>rl<strong>and</strong> Brown, A., 1960, Geology <strong>of</strong> <strong>the</strong> Rocher Deboule Range: British Columbia Department <strong>of</strong> Mines <strong>and</strong> Petroleum Resources Bulletin 43, 78 p. Su<strong>the</strong>rl<strong>and</strong> Brown, A., Cathro, R.J., Panteleyev, A., <strong>and</strong> Ney, C.S., 1971. Metallogeny <strong>of</strong> <strong>the</strong> Canadian Cordillera; in Canadian Institute <strong>of</strong> Mining <strong>and</strong> Metallurgy, Bulletin, v. 64, no. 709, p. 121-145. Su<strong>the</strong>rl<strong>and</strong> Brown, A.,1968, Geolagy <strong>of</strong> <strong>the</strong> Queen Charlotte Isl<strong>and</strong>s, British Columbia: Bhtish Caiumbb Department <strong>of</strong> Mines <strong>and</strong> Petroleum Resowoes, Bulletin 54,226 p. Swainbank, R.C., Bundtzen, T.K., <strong>and</strong> Wood, 3.. 1991, Mska's mineral industry 1990: Division <strong>of</strong> Geological end Geophysical Surveys, Special Report 45, 78 p. Swainbank, R.C., Bundtzen, T.K., Clough, A.H., Heming, M.M., <strong>and</strong> Hansen, E.W., 1995, <strong>Alaska</strong>'s mineral induatry 1994. <strong>Alaska</strong> Division <strong>of</strong> Geobgicd <strong>and</strong> Geophysical Surveys Special Report 49,75 p. Swainbank, R.C., Smith, T.E., <strong>and</strong> Turner, D.L., 1978, Gedogy <strong>and</strong> K-Ar age <strong>of</strong> mineralized intruslv@ rocks from <strong>the</strong> Chulitna mining district, central Alaeka. <strong>Alaska</strong> Division <strong>of</strong> Geological <strong>and</strong> Geophysical Swveys Gedogic Report 55, p. 23-28. 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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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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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Origin of and Tectonic Controls for
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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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Origin of and Tectonic Controls for
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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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Origin of and Tectonic Controls for
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Origin of and Tectonic Controls for
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Origin of and Tectonic Controls for
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hosted in the Yarkhodon subterrane
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origin of the younger Triassic(?) B
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Origin of and Tectonic Controls for
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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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Origin of and Tectonic Controls for
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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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Origin of and Tectonic Controls for
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Figure 46. Lawyers Au-Ag epitiefmel
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Origin of and Tectonic Controls for
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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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Origin of and Tectonic Controls for
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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
- 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
- Page 190 and 191:
- . --- 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
- Page 198 and 199:
- Origin of and Tectonic Controls f
- Page 200 and 201:
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
- Page 216 and 217:
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
- Page 226 and 227:
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
- Page 248 and 249:
closure, the Chukotka supertca&c wa
- Page 250 and 251:
- Mgh anglefau#or prsminant Fitwar
- Page 252 and 253:
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
- Page 260 and 261:
Eastern Asia-Arctic Metallogenic Be
- Page 262 and 263:
Valunistoe Au-Ag Epithermal Vein De
- Page 264 and 265:
Lost River Sn-W Skarn and Sn Greise
- Page 266 and 267:
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
- Page 274 and 275:
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:
Origin of and Tectonic Controls for
- 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:
Origin of and Tectonic Controls for
- Page 290 and 291:
CRETACEOUS Mount Leonard St& gueYtr
- Page 292 and 293:
n pJ pRanens. Pd-dc i3 Meeomic .---
- Page 294 and 295:
Figure 120. Huckleberry porphyry Cu
- Page 296 and 297:
0.15% Cu (ox), 0.127 g/t Au, and 0.
- Page 298 and 299:
Zone are 188 million tonnes grading
- Page 300 and 301:
Kitsault (B.C. Moly) Porphyry Mo De
- Page 302 and 303:
million tonnes grading 0.42% Cu, 0.
- Page 304 and 305:
extension. The Coryell Suite is int
- Page 306 and 307:
elated deposits. Forming in the bac
- Page 308 and 309:
Metallogenic Belts Formed in Tertia
- Page 310 and 311:
Hg Deposits Hg deposits occur throu
- Page 312 and 313:
Maletoivayam Sulfur-Sulfide Deposit
- Page 314 and 315:
Origin of and Tectonic Controls for
- 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
- Page 340 and 341: 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: Geology of the Liese zone, Pogo pro
- 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 403 and 404: Deposit Name Mineral Deposit Model
- Page 405 and 406: Deposit Name Mineral Deposit Model
- Page 407 and 408: Deposit Name Mineral Deposit Model
- Page 409 and 410: Deposit Name Mineral Deposit Model
- Page 411 and 412: Deposit Nmme Mineral Deposit Model
- Page 413 and 414: Deposit Name Mineral Deposit Model
- Page 415 and 416: Deposit Name Mineral Deposit Model
- Page 417 and 418:
Deposit Name Mineral Deposit Model
- Page 419 and 420:
p;. ;A'..* Deposit Name Mineral Dep
- Page 421 and 422:
Deposit Name Mineral Deposit Model
- Page 423 and 424:
Deposit Name Mineral Deposit Model
- Page 425:
De~osit Name Mineral Deposit Model