USGS Professional Paper 1697 - Alaska Resources Library

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324 Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera Plyashkevich, A.A., 1990, On canfieldite-type tin-silverpolymetallic mineralization: Ore formations of the U.S.S.R. Northeast: U.S.S.R. Academy of Sciences, North-Eastern Interdisciplinary Research Institute, Magadan, p . 141-151. Pokazanyev, V.P., 1976a, Arykymbin gold-bearing volcanotectonic structure in south-western Omolon massif: Kolyma, no. 3, p. 38-39 (in Russian). Pokazanyev, V.P., 1976b, On Paleozoic metallogeny of gold in Omolon massif: Kolyma, no. 4, p. 42-44 (in Russian). Pollack, John, 1997, Summary report of the Lantarsky Concession, Khabarovsk Krai, Russian Federation: Amurcan Limited Status Report, 45 pages. Popeko, V.A., 1995, Magmatic formations and mineralization in the Okhotsk-Chukotka volcanic belt, in Bundtzen, T.K., Fonseca, A.L., and Mann, Roberta, eds., The Geology and Mineral Deposits of the Russian Far East: Alaska Miners Association, Glacier House Publications, Anchorage, Alaska, p. 19-28. Poulsen, K.H., 1996, Carlin-type gold deposits and their potential occurrence in the Canadian Corillera, in Current Research 1996-A: Geological Surey of Canada, p. 1-9. Pozdeev, A.I., 1986, Late Paleogenic stage in development of Koryak upland and some other regions of the Pacific belt: Tikhookeanskaya Geologiya, no. 4, p. 49-57 (in Russian). Pozdeev, A.I., 1990, Volcanic epochs, volcanic belts and metallogeny of Koryak-Kamchatka region: Volcanism (evolution, geodynamics, and ores): Nedra, Moscow, p.266-276 (in Russian). Pratt, W.P., ed., 1981, Metallic mineral-resource potential of the Rolla quadrangle, Missouri, as appraised in September 1980: U.S. Geological Survey Open-File Report 81-518, 77 p., 11 plates, scale 1:250,000. Preto, V.A., 1972, Geology of Copper Mountain; British Columbia Department of Mines, and Petroleum Resources, Bulletin 59, 87 p. Preto, V.A., and Schiarizza, P., 1985, Geology and mineral deposits of the Adams Plateau-Clearwater region, in Tempelman-Kluit, J.D., ed., Field Guides to Geology and Mineral Deposits in the Southern Canadian Cordillera: Geological Society of America, Cordilleran Section Meeting, Vancouver, Field Trip 16, p. 1-11. Preto, V.A., and Tidsbury, A.D., 1971, Magnum Mine: in Geology, Exploration and Mining in British Columbia 1971: British Columbia Department of Mines, and Petroleum Resources, p. 81-89. Radkevich E.A., 1984, Metallogenic zones of the Pacific ore belt: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, 192 p. (in Russian). Radkevich, E.A., ed., 1991, Pacific margin of Asia: Metallogenesis: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, 204 p. (in Russian). Radkevich E.A., Moiseenko V.G., Molchanov P.Ya., Melnikov V.D., and Fat’yanov I.I., 1969, The Tokur deposit as a representative of a quartz low-sulfide formation, in Radkevich, E.A., ed., Gold formations of the Russian Far East: Nauka, Moscow, p. 61-73. Raevskaya, I.S., Kalinin, A.I., and Natalenko, V.E., 1977, On mineral formation stages in gold-silver deposit: Kolyma, no. 5, p. 15-20 (in Russian). Ramthun, Alexander, Brandon, M.T., and Ring, Ewe, 1997, Preservation of sedimentary fabrics in the footwall of the large-slip vatyna thrust, Kamchatka, Russian Far East [abs.]: Geological Society of America Abstracts with Program, v. 29, p. 58. Ratkin, V.V., 1991, On the relationship of skarn borosilicate and polymetallic ores of the Dalnegorsk ore district, in Shcheka, S.A., ed., Ore deposits of the Russian Far East— Mineralogical criteria for prediction, prospecting, and estimation: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, 112 p. (in Russian). Ratkin, V., 1995, Pre- and postaccretionary metallogeny of the southern Russian Far East: Resource Geology, Special Issue No. 18, p. 127-133. Ratkin, V.V., and Khanchuk, A.I., 1995, Lode mineral deposits of the southern Russian Far East, in Bundtzen, T.K., Fonseca, A.L., and Mann, Roberta, eds., The Geology and Mineral Deposits of the Russian Far East: Alaska Miners Association, Glacier House Publications, Anchorage, Alaska, p. 85-89. Ratkin V.V., Khetchikov, L.N., and Dmitriev, V.E., 1992, On the role of colloids and paleohydrothermal cavities for the formation of rhythmically banded ore of the Dalnegorsk borosilicate deposit: Doklady Akademii Nauk SSSR, v. 325, p. 1214-1217. (in Russian). Ratkin, V.V, and Watson, B.N., 1993, Dalnegorsk borosilicate deposits: Geology and sources of boron on the basis of isotope data: Tikhookeanskaya Geologiya, no. 6, p. 95-102 (in Russian). Ratkin, V.V., Simanenko, L.F., Kuznetsov D.N., and Korol, R.V., 1990, Tin-zinc ores of East Sikhote-Alin volcanic belt: Geologiya Rudnykh Mestorozhdeniy, no.2, p. 68-77 (in Russian). Ratkin, V.V., Simanenko, L.F., and Logvenchev, P.I., 1991, Mineralogical and geochemical zoning of skarn and vein polymetallic deposits of the Dalnegorsk district as a basis for local prediction of the vertical distribution of the deposit, in Shcheka, S.A., ed., Ore deposits of the Russian
Far East—Mineralogical criteria for prediction, prospecting, and estimation: U.S.S.R. Academy of Sciences, Far East Geological Institute, Vladivostok, p. 33-35 (in Russian). Ratkin, V.V, Watson, B.N., 1993, Dalnegorsk borosilicate deposits—Geology and sources of boron on the basis of isotope data: Tikhookeanskaya Geologiya, no. 6, p. 95-102 (in Russian). Ray, R.G., 1954, Geology and ore deposits of the Willow Creek mining district, Alaska: U.S. Geological Survey Bulletin 1004, 86 p. Ray, G.E., 1986, Gold associated with a mid-Tertiary plutonic event in the Harrison Lake area, southwestern British Columbia (92 G/9; 92 H/3,4,5,6,12), in Geological Fieldwork 1985: British Columbia Ministry of Energy, Mines, and Petroleum Resources Paper 1986-1, p. 95-97. Ray, G.E., 1991, Vein gold mineralization related to mid-Tertiary plutonism, Harrison Lake, British Coilumbia: Economic Geology, v. 86, p. 883-891. Ray, G.E., and Dawson, G.L., 1994, The geology and mineral deposits of the Hedley gold skarn district, southern British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum Resources Bulletin no. 87, 156 p. Ray, G.E., and Dawson, K.M., 1998, Mineralized skarns in the Canadian Cordillera, in Lentz, D.R., ed., Mineralized Intrusion-Related Skarn Systems, Mineralogical Association of Canada, Short Course Volume 26, p. 475-518. Ray, G.E; Grond, H.C; Dawson, G.L; and Webster, I.C.L., 1992, The Mount Riordan (Crystal Peak) garnet skarn, Hedley District, southern British Columbia: Economic Geology, v.87, no.7, p.1862-1876. Ray, G.E., and Webster, I.C.L., 1991, An overview of skarn deposits, in McMillan, W.J. and others, eds., Ore Deposits, Tectonics and Metallogeny in the Canadian Cordillera: British Columbia, Ministry of Energy, Mines, and Petroleum Resources Paper 1991-4, p. 213-252. Ray, G.E., and Webster, I.C.L., 1997, Skarns in British Columbia: British Columbia Ministry of Energy and Mines Bulletin 101, 260 p. Ray, G.E., Webster, I.C.L., Dawson G.L. and Ettlinger, A.D., 1993, A geological overview of the Hedley Gold Skarn district, southern British Columbia (92H), in Geological Fieldwork 1992: British Columbia Ministry of Energy, Mines, and Petroleum Resources Paper 1993-1, p. 269-280. Ray, R.G., 1954, Geology and ore deposits of the Willow Creek mining district, Alaska: U.S. Geological Survey Bulletin 1004, 86 p. Read, J.J., 1985, Gold-quartz mineralization at the Big Hurrah mine, Seward Peininsula, Alaska [abs.]: Geological Society of America Abstracts with Programs, v. 17, no. 6, p. 402. References Cited 325 Read, J.J., and Meinert, L.D., 1986, Gold-bearing quartz vein mineralization at the Big Hurrah mine, Seward Peninsula: Economic Geology, v. 81, p. 1760-1774. Read, P.B., and Monger, J.W.H., 1976, Pre-Cenozoic volcanic assemblages of the Kluane and Alsek ranges, southwestern Yukon Territory: Geological Survey of Canada Open File 381, 96 p. Rebagliati, C.M., Bowen, B.K., Copeland, D.J., and Niosi, D.W.A., 1995, Kemess South and Kemess North porphyry gold-copper deposits, northern British Columbia, in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining and Metallurgy, Special Volume 46, p. 377-396. Reed, J.C., and Coats, R.R., 1941, Geology and ore deposits of the Chichagof mining district, Alaska: U.S. Geological Survey Bulletin 929, 148 p. Reed, B.L., and Eberlein, G.D., 1972, Massive sulfide deposits near Shellabarger Pass, southern Alaska Range: U.S. Geological Survey Bulletin 1342, 45 p. Reed, B.L., and Lanphere, M.A., 1969, Age and chemistry of Mesozoic and Tertiary plutonic rocks of south-central Alaska: Geological Society of America Bulletin, v. 80, no. 1, p. 23-44. Reed, B.L., and Lanphere, M.A., 1973, Alaska-Aleutian Range batholith: Geochronology, chemistry, and relation to Circum-Pacific plutonism: Geological Society of America Bulletin, v. 84, p. 2583-2610. Reed, B.L., Menzie, W.D., and McDermott, M., Root, D.H., Scott, W., and Drew, L.J., 1989, Undiscovered lode tin resources of the Seward Peninsula, Alaska: Economic Geology, v. 84, p. 1936-1947. Reed, B.L., Miesch, A.T., and Lanphere, M.A., 1983, Plutonic rocks of Jurassic age in the Alaska-Aleutian Range batholith—Chemical variations and polarity: Geological Society of America Bulletin, v. 94, p. 1232-1240. Reed, J.C., and Coats, R.R., 1941, Geology and ore deposits of the Chichagof mining district, Alaska: United States Geological Survey Bulletin 929, 148 p. Reed, J.J., and Meinhart, L.D., 1986, Gold-bearing quartz vein mineralization at the Big Hurrah mine, Seward Peninsula, Alaska: Economic Geology, v. 81, p. 1,760-1,774. Reesor, J.E., 1973, Geology of the Lardeau Map-area, east half, British Columbia: Geological Survey of Canada Memoir 369, p. 92-117, scale 1:250,000. Rhys, D.A., and Godwin, C.I., 1992, Preliminary structural interpretation of the Snip Mine (104B/11, in Geological Fieldwork 1991: British Columbia Ministry of Energy, Mines, and Petroleum Resources Paper 1992-1, p. 549-554.
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USGS Prepared in collaboration with
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U.S. Department of the Interior Gal
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iv Hart River SEDEX Zn-Cu-Ag Deposi
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vi Specific Events for Middle Throu
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viii Metallogenic Belts Formed Duri
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x Origin of and Tectonic Controls f
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xii Toodoggone Metallogenic Belt of
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xiv Slate Creek Serpentinite-Hosted
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xvi Left Omolon Belt of Porphyry Mo
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xviii Origin of and Tectonic Contro
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xx Chukotka Metallogenic Belt of Au
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xxii Plutonic Rocks Hosting East-Ce
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xxiv Skeena Metallogenic Belt of Po
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xxvi Bee Creek Porphyry Cu Deposit
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xxviii 36. Wellgreen gabbroic Ni-Cu
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xxx 87. Partizanskoe Pb-Zn skarn de
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Metallogenesis and Tectonics of the
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format (Nokleberg and others, 1996)
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logenesis of the region (1) subduct
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Subterrane—A fault-bounded unit w
Page 41 and 42:
dilemma consists of two conflicting
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2 to 20 m thick. A related dolomite
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Lantarsky-Dzhugdzhur Metallogenic B
Page 47 and 48:
Origin of and Tectonic Controls for
Page 49 and 50:
Metallogenic Belts Formed During Pr
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as at Oz, Monster, and Tart, may al
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Monashee Metallogenic Belt of Sedim
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Clark Range Metallogenic Belt of Se
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in addition to the Fe deposits. Min
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study) consists of lenses, from 100
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Omulev Austrian Alps W Deposit The
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ock, including coarse clastic rock,
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lative metalliferous brines in a re
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Prince of Wales Island Metallogenic
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suite of deposits and host rocks ar
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margin of the North American Craton
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newly created terranes migrated int
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(Ryazantzeva and Shurko, 1992). The
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tonnes Au and an average grade of a
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mafic and felsic metavolcanic rocks
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intrusion from about 402 to 366 Ma
Page 83 and 84:
Page 85 and 86:
mentary rocks of the Cambrian to De
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(Preto and Schiarizza, 1985; Schiar
Page 89 and 90:
Page 91 and 92:
ate and clastic rocks and volcanicl
Page 93 and 94:
(Nokleberg and others, 1994c, 1997c
Page 95 and 96:
Berezovka River Metallogenic Belt o
Page 97 and 98:
Page 99 and 100:
Finlayson Lake Metallogenic Belt of
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and barite in siliceous black turbi
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Windermere Creek (Western Gypsum) C
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(NX, DL, MY), Viliga (VL), and Zolo
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South of the main east-west-trendin
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ated subduction zone in the Wrangel
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icite-biotite-quartz bodies in frac
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Canada Cordillera. The granitoid ro
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Viliga (VL) passive continental-mar
Page 117 and 118:
32; tables 3, 4) occurs along the n
Page 119 and 120:
superterrane, consists mainly of ma
Page 121 and 122:
ers, 1994c, 1997c). In southern Bri
Page 123 and 124:
mental volcanic rocks of intermedia
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a resource of 34.3 million tonnes o
Page 127 and 128:
potassic zone. Combined estimated p
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and quartz monzodiorite stock and s
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and Omolon (OM) cratonal terranes,
Page 133 and 134:
in volcanic and volcaniclastic rock
Page 135 and 136:
minor calcite, and sporadic pyrite
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supergene blanket are interpreted a
Page 139 and 140:
deposits and occurrences consist of
Page 141 and 142:
onto the Omulevka terrane to form t
Page 143 and 144:
superterrane. This belt is interpre
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to form along the leading edge of t
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quartz, and is virtually not associ
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deposits are at Terrassnoe and Kuna
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Peschanka Porphyry Cu-Mo Deposit Th
Page 153 and 154:
The belt is hosted in the Late Jura
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in a island arc that was tectonical
Page 157 and 158:
and Early Cretaceous Koyukuk island
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The deposit consists of disseminate
Page 161 and 162:
The Orange Hill deposit contains an
Page 163 and 164:
49; tables 3, 4) (Foley and others,
Page 165 and 166:
locally Late Triassic marine volcan
Page 167 and 168:
gold in a gangue of quartz, calcite
Page 169 and 170:
Verkhoyansk granite belt, which int
Page 171 and 172:
metallogenic belts are interpreted
Page 173 and 174:
assemblages, which may have been mo
Page 175 and 176:
during hypogene and supergene alter
Page 177 and 178:
collision and regional thrusting, t
Page 179 and 180:
Yur Au Quartz Vein Deposit The smal
Page 181 and 182:
phase has a Rb-Sr isotopic age of 1
Page 183 and 184:
sian Northeast. The belt is hosted
Page 185 and 186:
Host Granitoid Rocks and Associated
Page 187 and 188:
that are up to 600-1,500 m long, av
Page 189 and 190:
Metallogenic Belts Formed During La
Page 191 and 192:
y partly coeval plutons that range
Page 193 and 194:
tion is interpreted as occuring by
Page 195 and 196:
the Badzhal-Ezop and Khingan parts
Page 197 and 198:
and comagmatic with volcanic rocks;
Page 199 and 200:
as interpreted for the Rock Creek d
Page 201 and 202:
source (Yeo, 1992). The Blow River
Page 203 and 204:
2000). The spatial location of the
Page 205 and 206:
to the east in the central Yukon Te
Page 207 and 208:
occur in a 30-km-long belt along ir
Page 209 and 210:
The Emerald deposit has produced ap
Page 211 and 212:
Metallogenic-Tectonic Model for Ear
Page 213 and 214:
cham oceans were closed, and the Ch
Page 215 and 216:
greisenized Mesozoic granite that i
Page 217 and 218:
composition magmatic bodies (with a
Page 219 and 220:
Page 221 and 222:
to Albian pelecypods (Nokleberg and
Page 223 and 224:
quartz-arsenopyrite-pyrrhotite, pol
Page 225 and 226:
thermally altered to siliceous and
Page 227 and 228:
These ore bodies are as much as 1 m
Page 229 and 230:
Eastern Asia-Arctic Metallogenic Be
Page 231 and 232:
Demin, and Krasilnikov, 1974; Nekra
Page 233 and 234:
10 percent Cu, as much as 0.92 perc
Page 235 and 236:
pyrite, pyrite, galena, sphalerite,
Page 237 and 238:
content decreases with depth, as do
Page 239 and 240:
azdelnoye, (2) porphyry Sn deposits
Page 241 and 242:
Karalveem Au Quartz Vein Deposit Th
Page 243 and 244:
Democrat (Mitchell Lode) Granitoid-
Page 245 and 246:
with high-temperature and high-pres
Page 247 and 248:
chalcocite and covellite and also h
Page 249 and 250:
cum-North Pacific, (2) completion o
Page 251 and 252:
(6) In the Paleocene (about 56 to 6
Page 253 and 254:
sists of cinnabar and metacinnabari
Page 255 and 256:
Eastern Asia-Arctic Metallogenic Be
Page 257 and 258:
groups of deposits are interpreted
Page 259 and 260:
Indian Mountain and Purcell Mountai
Page 261 and 262:
and southeastern Alaska (Moll and P
Page 263 and 264:
Nokleberg and others, 1995a; Bundtz
Page 265 and 266:
g/t Au or 368.2 Au gold. The deposi
Page 267 and 268:
wim Group and altered mafic dikes.
Page 269 and 270:
Mount Nansen porphyry Cu-Mo deposit
Page 271 and 272:
A Map 450 500 550 Cross section Dik
Page 273 and 274:
Cretaceous and early Tertiary conti
Page 275 and 276:
deposits, at Chichagoff and Hirst-C
Page 277 and 278:
others, 1994c, 1997c). The signific
Page 279 and 280:
tonnes grading 0.53 percent Ni, 0.3
Page 281 and 282:
with a 0.25 percent cut-off. The de
Page 283 and 284:
Bulkley Metallogenic Belt of Porphy
Page 285 and 286:
Red Rose W-Au-Cu-Ag Polymetallic Ve
Page 287 and 288:
ish Columbia and consists of severa
Page 289 and 290:
during back-arc extension or transt
Page 291 and 292:
stocks and dikes, is associated wit
Page 293 and 294:
etrograde minnesotaite (Fe talc), F
Page 295 and 296:
Specific Events for Early to Middle
Page 297 and 298:
of fractured and faulted Permian-Tr
Page 299 and 300:
sists of a mineralized fracture zon
Page 301 and 302:
dolomite. Wall rock alteration incl
Page 303 and 304:
elt of late Tertiary plutons that a
Page 305 and 306: plates that exhibit magnetic anomal
Page 307 and 308: stages (Petrenko, 1999): (1) In the
Page 309 and 310: mon. The deposit is of medium size
Page 311 and 312: Metallogenic-Tectonic Model for Lat
Page 313 and 314: The origin of the Hg deposits of th
Page 315 and 316: margin or island-arc tectonic envir
Page 317 and 318: Columbia: Implicatons for the Middl
Page 319 and 320: Bazard, D.R., Butler, R.F., Gehrels
Page 321 and 322: Bradley, D.C., Haeussler, P.J., and
Page 323 and 324: Bundtzen, T.K., Laird, G.M., Caluti
Page 325 and 326: Cecile, M.P., 1982, The lower Paleo
Page 327 and 328: Debari, S.M., and Coleman, R.G., 19
Page 329 and 330: U.S. Bureau of Land Management Open
Page 331 and 332: Cordilleran Orogen in Canada: Geolo
Page 333 and 334: Goldfarb, R., Hart, C., Miller, M.,
Page 335 and 336: Grove, E.W., 1986, Geology and mine
Page 337 and 338: Høy, T., 1982a, Stratigraphic and
Page 339 and 340: Jones, D.L., Silberling, N.J., Cone
Page 341 and 342: Kutyev, F. Sh., Baikov, A.I., Sidor
Page 343 and 344: Shield—Ultramafic magma and its m
Page 345 and 346: Manns, F.T., 1981, Stratigraphic as
Page 347 and 348: Miller, M.L., and Bundtzen, T.K., 1
Page 349 and 350: Mortimer, N., 1987, The Nicola Grou
Page 351 and 352: Noble, S.R., Spooner, E.T.C., and H
Page 353 and 354: Canada Annual Meeting, Saskatoon, S
Page 355: Perello, J.A., Fleming, J.A., O’K
Page 359 and 360: Roeske, S.M., Mattinson, J.M., and
Page 361 and 362: Schmidt, J.M., and Zierenberg, R.A.
Page 363 and 364: formation occurrences: Materialy po
Page 365 and 366: Struik, L.C., 1986, Imbricated terr
Page 367 and 368: Valuy, G., and Rostovsky, F., 1988,
Page 369 and 370: Wolfe, W.J., 1995, Exploration and
Page 371 and 372: Appendix Table 1. Mineral deposit m
Page 373 and 374: Table 2 Summary of correlations and
Page 375 and 376: Table 2—Continued Unit(s) and Cor
Page 377 and 378: Table 2—Continued Unit(s) and Cor
Page 379 and 380: Table 3—Continued Metallogenic Be
Page 399 and 400: Table 4. Significant lode deposits,
Page 401 and 402: Table 4—Continued Appendix 369 De
Page 403 and 404: Table 4—Continued Tracy Metalloge
Page 405 and 406: Table 4—Continued Appendix 373 In
Page 407 and 408:
Table 4—Continued Deposit Name Mi
Page 409 and 410:
Table 4—Continued Mainits Metallo
Page 411 and 412:
Page 413 and 414:
Table 4—Continued Appendix 381 De
Page 415 and 416:
Table 4—Continued Whitehorse Meta
Page 417 and 418:
Page 419 and 420:
Table 4—Continued Appendix 387 De
Page 421 and 422:
Table 4—Continued Appendix 389 LA
Page 423 and 424:
Page 425 and 426:
Table 4—Continued Surprise Lake M
Page 427 and 428:
Table 4—Continued Sredinny Metall
Page 429:
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