USGS Professional Paper 1697 - Alaska Resources Library

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312 Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera McCoy, D., Newberry, R.J., and Layer, P., 1997, Plutonic-related gold deposits of interior Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska: Economic Geology Monograph 9, p. 191-241. MacDonald, A.J., Spooner, E.T.C., and Lee, G., 1995, The Boss Mountain molybdenum deposit, central 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. 691-698. Macdonald, R.W.J., Barrett, T.J., and Sherlock, R.L., 1996, Geology and lithogeochemistry at the Hidden Creek massive sulphide deposit, Anyox, west-central British Columbia: Exploration and Mining Geology, v. 5, no. 4, p. 369-398. MacIntyre, D.G., 1982, Geologic setting of recently discovered barite-sulphide deposits of northeast British Columbia; Canadian Institute of Mining and Metallurgy Bulletin, v. 75, no. 840, p. 99-113. MacIntyre, D.G., 1985, Geology and mineral deposits of the Tahtsa Lake district, west-central British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum Resources Bulletin 75, 82 p. MacIntyre, D.G., 1991, Sedex-sedimentary exhalative 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. 25-70. MacIntyre, D.G., Geology, geochemistry and mineral deposits of the Akie River area, northeast British Columbia: British Columbia Ministry of Energy and Minerals Divisions, Geological Survey Branch Bulletin, 91 p. MacIntyre, D.G., Mihalynuk, M.G., and Smith, M.T., 1993, Tatshenshini Project, northwestern British Columbia 114P/11, 12, 13, 14; 114O/9, 10, 14, 15 & 16), Part D: Mineral Inventory update (114P and 114O), in Fieldwork 1992: British Columbia Ministry of Energy, Mines, and Petroleum Resources Paper 1993-1, p. 217-229. MacKevett, E.M., Jr., 1963, Geology and ore deposits of the Bokan Mountain uranium-thorium area, southeastern Alaska: U.S. Geological Survey Bulletin 1154, 125 p. MacKevett, E.M., Jr., 1965, Ore controls at the Kathleen- Margaret (Maclaren River) copper deposit, Alaska: U.S. Geological Survey Professional Paper 501c, p. C116-C120. MacKevett, E.M., Jr., 1976, Mineral deposits and occurrences in the McCarthy quadrangle, Alaska: United States Geological Survey, Miscellaneous Field Study Map, MF-773-B, 2 sheets, scale 1:250,000. MacKevett, E.M., Jr., 1976, Mineral deposits and occurrences in the McCarthy quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-773B, 2 sheets, scale 1:250,000. MacKevett, E.M., Jr., 1978, Geologic map of the McCarthy quadrangle, Alaska: U.S. Geological Survey Miscellaneous Investigations Series Map I-1032, scale 1:250,000. MacKevett, E.M., Jr., Brew, D.A., Hawley, C.C., Huff, L.C., and Smith, J.G., 1971, Mineral resources of Glacier Bay National Monument, Alaska: U.S. Geological Survey Professional Paper 632, 90 p. MacKevett, E.M., Jr., Cox, D.P., Potter II, Robert W., and Silberman, M.L., 1997, Kennecott-type deposits in the Wrangell Mountains, Alaska: High-grade copper ores near a basalt-limestone contact, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska: Economic Geology Monograph 9, p. 66-89. MacKevett, E.M., Jr., and Plafker, George, 1974, The Border Ranges fault in south-central Alaska: U.S. Geological Survey Journal of Research, v. 2, no. 3, p. 323-329. MacKevett, E.M., Jr., Robertson, E.C., and Winkler, G.R., 1974, Geology of the Skagway B-3 and B-4 quadrangles, southeastern Alaska: U.S. Geological Survey Professional Paper 832, 33 p., 1 sheet, scale 1:63,360. Mackey, K.G., Fujita, K., Gunbina, L.V., Kovalev, V.N., Imaev, V.S., Koz’min, B.M., and Imaeva, L.P., 1997, Seismicity of the Bering Strait region—evidence for a Bering block: Geology, v. 25, p. 979-982. McMillan, W.J., 1973, Mount Coipeland Mine, in Geology, Exploration and Mining in British Columbia: British Columbia Ministry of Energy, Mines, and Petroleum Resources, p. 104-1123. McMillan, W.J., 1980, Geologic fieldwork, 1979; a summary of field activities: British Columbia Geological Divison Geological Fieldwork, no.1980-1, p.37-48. Macqueen, R.W., and Thompson, R.I., 1978, Carbonate hosted lead-zinc occurrences in northestern British Columbia, with emphasis on the Robb Lake deposit: Canadian Journal of Earth Sciences, v.15, p. 1737-1762. Madden-McGuire, D.J., Silberman, M.L., and Church, S.E., 1989, Geologic relationships, K-Ar ages, and isotopic data from the Willow Creek gold mining district, southern Alaska, in Keays, R.R., Ramsay, W.R.H., and Groves, D.I., eds., The geology of gold deposits—The perspective in 1988: Economic Geology Monograph 6, p. 242-251. Madu, B.E., Nesbitt, B.E., and Muehlenbachs, K., 1990, A mesothermal gold-stibnite-quartz vein occurrence in the Canadian Cordillera: Economic Geology, v.85, p. 1260-1286. Mahoney, L.R., 1977, Geology of Pemberton (92J) map area, British Columbia: Geological Survey of Canada, Open File Map 482, scale 1:250,000.
Manns, F.T., 1981, Stratigraphic aspects of the Silurian-Devonian sequence hosting zinc and lead mineralization near Robb Lake, northeastern British Columbia: Toronto, Ontario, University of Toronto, Ph.D. dissertation, 345 p. Marakuchev, A.A., Emel’yanenko, E.P., and Nekrasov, I.Ya., 1990, The original concentric-zoned structure of the Kondyor alkali-ultramafic massif: Doklady Akademii Nauk SSSR, v. 311, no.1, p.167-170 (in Russian). Markov, M.S., Nekrasov, G.E., and Palandzhyan, S.A., 1982, Ophiolite and melanocratic basement of the Koryak Highlands—Essay on tectonics of the Koryak Highlands: Nauka, Moscow, p. 30-70 (in Russian). Marriott, C., 1992, Developing the Polaris Taku gold deposit, Abstracts of technical presentations: Geological Society of the Canadian Instritute of Mining, Metallurgy, and Petroleum, Second Annual Field Conference, Sept. 28, 29 1992, Kamloops, British Columbia Martin, G.C., and Katz, F.J., 1912, A geologic reconnaissance of the Iliamna region, Alaska: U.S. Geological Survey Bulletin 485, 138 p. Mayfield, C.F., Tailleur, I.L., and Ellersieck, Inyo, 1983, Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska: U.S. Geological Survey Open-File Report 83-779, 58 p., 5 sheets, scale 1:1,000,000. McCaffrey, R., and Abers, G.A., 1991, Orogeny in arc-continent collision: the Banda arc and western New Guinea: Geology, v. 19, p. 563-566. McClay, K.R., and Bidwell, G.E., 1986, Geology of the Tom deposit, Macmillan Pass, Yukon, in Morin, J.A., ed., Mineral deposits of Northern Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 37, p. 100-114. McClelland, W.C., Gehrels, G.E., and Saleeby, J.B., 1992a, Upper Jurassic-Lower Cretaceous basinal strata along the Cordilleran margin—implications for the accretionary history of the Alexander-Wrangellia-Peninsular terrane: Tectonics, v. 11, p. 832-835. McClelland, W.C., Gehrels, G.E., Samson, S.D., and Patchett, P.J., 1991, Protolith relations of the Gravina belt and Yukon- Tanana terrane in central southeastern Alaska: Journal of Geology, v. 100, p. 107-123. McClelland, W.C., Gehrels, G.E., Samson, S.D., and Patchett, P.J., 1992b, Structural and geochronologic relations along the western flank of the Coast Mountains batholith—Stikine River to Cape Fanshaw, central southeastern Alaska: Journal of Structural Geology, v. 14, p. 475-489. McCoy, D., Newberry, R.J., Layer, P., DiMarchi, J.J., Bakke, A., Masterman, J.S., and Minehane, D.L., 1997, Plutonic-related gold deposits of interior Alaska, in Goldfarb, R.J., and Miller, References Cited 313 L.D., eds., Mineral deposits of Alaska: Economic Geology Monograph 9, p. 191-241. McDougall, J.J., 1976, Catface, in Sutherland Brown, A., ed., Porphyry Deposits of the Canadian Cordillera: Canadian Institute of Mining and Metallurgy Special Volume 15, p. 299-310. McMillan, W.J., 1973, Mount Copeland Mine, in Geology, Exploration and Mining in British Columbia 1973: British Columbia Ministry of Energy, Mines, and Petroleum Resources, p. 104-113. McMillan, W.J., 1980, CC prospect, Chu Chua Mountain: British Columbia Ministry of Energy and Mines, Geological Fieldwork 1979, Paper 1980-1, p. 37-48. McMillan, W.J., 1985, Geology and ore deposits of the Highland Valley camp: Geological Association of Canada, Mineral Deposits Division, Field Guide and Reference Manual Series, No. 1, 121 p. McMillan, W.J., 1991, Porphyry deposits in the Canadian Cordillera, 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. 253-276. McMillan, W.J., 1983, Granite Creek property (92O/3W), in Geology in British Columbia, 1976: British Columbia Ministry of Energy, Mines, and Petroleum Resources, p. 67-84. McMillan, W.J., Thompson, J.F.H., Hart, C.J.R., and Johnston, S.T., 1995, Regional geological and tectonic setting of porphyry deposits in British Columbia and Yukon Territory; in Schroeter, T.G., ed., Porphyry Deposits of the Northwestern Cordillera of North America: Canadian Institute of Mining and Metallurgy Special Volume 46, p. 20-39. McMechan, M.E., 1981, The middle Proterozoic Purcell Supergroup in the southwestern Rocky and southeastern Purcell Mountains, British Columbia and the initiation of the Cordilleran miogeocline, southern Canada and adjacent United States: Bulletin of Canadian Petroleum Geology, v. 29, p. 583-621. Meinert, L.D., 1986, Gold in skarns of the Whitehorse Copper Belt, southern Yukon, in Yukon Geology, v. 1: Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, p. 19-43. Melis, A.L., and Clifford, K.L., 1987, Golden Bear - Process alternatives, testing and selection for a refractory British Columbia gold ore: Northwest Miners Association, Annual Meeting, Spokane, 1987. Melkomukov, V.N., and Zaitsev, V.P., 1999, Platinum placers in the Galmeononsky-Seinavsky knot, Koryak-Kamchatka Province: Platinum of Russia and Problems of Development of the Platinum Metals Resource in the 21st Century: Collection of Transactions Russia Academy of Sciences, Khabarovsk, v. 3, 352 p. (in Russian).
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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
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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
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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
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(Nokleberg and others, 1994c, 1997c
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Berezovka River Metallogenic Belt o
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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
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superterrane, consists mainly of ma
Page 121 and 122:
ers, 1994c, 1997c). In southern Bri
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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,
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in volcanic and volcaniclastic rock
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minor calcite, and sporadic pyrite
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supergene blanket are interpreted a
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deposits and occurrences consist of
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onto the Omulevka terrane to form t
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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
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The belt is hosted in the Late Jura
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in a island arc that was tectonical
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and Early Cretaceous Koyukuk island
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The deposit consists of disseminate
Page 161 and 162:
The Orange Hill deposit contains an
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49; tables 3, 4) (Foley and others,
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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
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metallogenic belts are interpreted
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assemblages, which may have been mo
Page 175 and 176:
during hypogene and supergene alter
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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: Shield—Ultramafic magma and its m
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 and 356: Perello, J.A., Fleming, J.A., O’K
Page 357 and 358: Far East—Mineralogical criteria f
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 395 and 396:
Table 3—Continued Metallogenic Be
Page 397 and 398:
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:
Page 415 and 416:
Table 4—Continued Whitehorse Meta
Page 417 and 418:
Page 419 and 420:
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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