1 edition of Geochemical study of gold-quartz veins, Red Lake gold camp, northwest Ontario found in the catalog.
Geochemical study of gold-quartz veins, Red Lake gold camp, northwest Ontario
Written in English
|LC Classifications||QE 516 L192 1984 thesis|
|The Physical Object|
|Number of Pages||69|
The Fortress veins may be the source for the gold in the Thompson Pup placer deposits. The southern end of the Fortress area is cut by the Solomon Shear Zone and contains gold and antimony mineralized quartz veins distinctly different from the Fortress trend veins. The lode exploration program consisted of a variety of field exploration work. Full text of "Mining World Index of Current Literature" See other formats.
and Sanborn-Barrie, M., , Timing of gold mineralization in the Diakow, L.J., and Metcalfe, P., , Geology of the Swannell ranges in the Red Lake gold camp, northwestern Ontario, Canada: New constraints vicinity of the Kemess copper-gold porphyry deposit, Attycelley Creek from U-Pb geochronology at the Goldcorp high-grade zone, Red Lake 5/5(1). Northwest Aluminum Specialties produces aluminum billet in a variety of alloys. The company's log-shaped cast billet products, which range in diameter from inches to 11 inches, can be used by customers in hot extrusion and hot or cold impact extrusion and as hot or cold forging stock.
In making up this table it is assumed that the rocks to a depth of ten miles are about 95 per cent of igneous type, that is, crystallized from molten magma, and about 5 per cent of sedimentary type, that is, formed from the weathering and erosion of igneous rocks or preëxisting sediments, and deposited in beds or layers, either by water or by air (see pp. ). Proceedings of the International Conferences on Basement Tectonics VOLUME 2 The titles published in this series are listed at the end a/this volume. BASEMENT TECTONICS 8 Characterization and Comparison of Ancient and Mesozoic Continental Margins Proceedings of the Eighth International Conference on Basement Tectonics.
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♥ Book Title: Geochemical study of gold-quartz veins, Red-Lake gold camp, northwest Ontario ♣ Name Author: Judy Sue LaKind ∞ Launching: Info ISBN Link: WISC ⊗ Detail ISBN code: ⊕ Number Pages: Total sheet ♮ News id: VWxbAAAAMAAJ Download File Start Reading.
The Red Lake gold camp (Fig. 2) preserves an extensiv e record of volcano-magmatic and sedimentary activity from to Ga, and evidence of multiple episodes of deformation. The Ganboke mineralized district in the Pala area in the southern part of Chad is largely located in the Precambrian greenstone belt.
northwest Ontario book The gold mineralization occurs commonly as auriferous quartz veins (< m thick) together with networks or stockworks, which are spacially associated with shear zones trending N30°–45°E within greenstone.
Paragenetic and micro-structural relationships of Cited by: 3. The stratified rocks straddling the Larder Lake-Cadillac Break historically have been subdivided into two volcanic and two sedimentary groups (Wilson, ).The older volcanic unit, composed mainly of ultramafic to mafic rocks with rare felsic units, is termed the Malartic Group in the eastern part of the area, while its equivalent in the western part is referred to as the Larder Lake Group.
Toronto, Ontario--(Newsfile Corp. - February 7, northwest Ontario book - Palamina Corp. (TSXV: PA) is a pure gold exploration company preparing for its inaugural drilling campaign on its high-grade Coasa Gold.
Dube B, Williamson K, McNicoll V, Malo M, Skulski T, Twomey T, Sanborn-Barrie M - Timing of Gold Mineralization at Red Lake, Northwestern Ontario, Canada: New Constraints from U-Pb Geochronology at the Goldcorp High-Grade Zone, Red Lake Mine and at the Madsen Mine; in Econ.
Geol. v99 pp. The primary geochemical dispersion halo may extend laterally for > m, and along strike for a few kilometres, from the gold orebody. A single geochemical parameter rarely defines an extensive.
Jasper, M.W., a, Geochemical investigations, Willow Creek southerly to Kenai Lake region, south central Alaska: Alaska Division of Mines and Minerals Geochemical Rep 47 p. Jasper, M.W., b, Geochemical investigations along the Valdez to Chitina highway in south central Alaska, Alaska Division of Mines and Minerals.
Issue 55 - 8 / Sulfur isotope investigation of the Gold-Quartz deposits of the Yellowknife District; Some ore occurrences of the Mississippi Valley type in Equatorial Africa, $ 10 Issue 58 - 5 / Some Vein-Wall Rock Relationships in the White Pine Mine, Ontonagon County, Michigan, $ 10 1.
Introduction. The genesis of vein-type to disseminated gold deposits, broadly classified as orogenic gold deposits (Groves et al.,Goldfarb et al., ) has remained genetic models for these deposits were evaluated in a recent review by Goldfarb and Groves ().Much attention has been focused on the source of auriferous by: A volume on gold was selected for a general review-type publication because of the importance of the gold mining industry in the s.
The officers and council of the Society of Economic Geologists authorized the preparation of this book on gold inand Dr. Lode gold deposits are one of the most M.J. and Crocket, J.H. () Geology of the East South C ore zone, Dickenson Mine, Red Lake.
In The Geology of Gold in Ontario, ed. Colvine, A.C. Ontario () Fluid access and fluid- wall rock interaction in the genesis of the Archaean gold-quartz vein deposit at Hunt mine, Kambalda, Western Cited by: Rift relocation -- a geochemical and geochronological investigation of a paleo-rift in northwest Iceland: Earth and Planetary Science Letters,Harker, A.
The Natural History of. Lindgren, Waldemar (a), The gold-quartz veins of Nevada City and Grass Valley districts, California: USGS 17th. Annual Report, part 2: ; Murdoch, Joseph & Robert W.
Webb (), Minerals of California, Centennial Volume (): California Division Mines & Geology Bulletin 84, ; Pemberton, H. Earl (), Minerals of. The Laverty Property is the most advanced; it is located one mile west of the town of Red Lake, Ontario and consists of six (6) patented Claims (KRL and ) on the boundary between Heyson and Dome Townships.
The Laverty Property is located within the heavily explored Red Lake gold camp. Gold-quartz vein from Red Mountain Mining District,Ouray County,Colorado,USA Pressure changes cause precious metal to deposit each tim The Largest and Most Significant Black Gem A mammoth carats “The Eternal Flame” is the largest and most significant black crystal ever found.
Listwanite (carbonated-serpentinite), commonly associated with high-grade lodegold mineralization, binds large quantities of the greenhouse gas carbon dioxide (CO₂).
At Atlin, B.C., listwanite distribution is controlled by a basal thrust fault and regional joint/fracture system with four steeply dipping sets. Carbonation proceeded via three sub-reactions fossilized as spatially distinct Cited by: 2. The veins range in thickness between and m, and were mined for gold between the late s andproducing some kg gold at an average grade at 30 g/t (Young b).
No copper. Gold quartz veins occur in rocks of all four major terranes, but the major deposits seem to a west-northwest-trending belt of gold deposits. Coarse-grained potassium feldspar that contains molybdenite and chalcopyrite, collected from a mine this near-surface geochemical study suggesting natuFile Size: 14MB.
BEDROCK SOURCE gold-quartz veins in PZ+MZ slate, schist, granite aureole t Au Williams () Cr3 dunite and pyroxenite intru sions t Pt met. 2 t Au post-J regolithic dunite,peridotite,picrite bodies t Pt met.
6 t Au TONNAGE H REFERENCES Selected examples of metalliferous alluvial placers (all considered Quaternary, unless marked T. This banner text can have markup.
web; books; video; audio; software; images; Toggle navigation.Ray, G.E., Dawson, G.L. & Simpson, G. () The Geology and controls of skarn mineralization In the Hedley gold camp Southern British Columbia* (92W8, ) British Columbia Ministry of Energy, Mines and Petroleum Resources.
Geological Fieldwork,Paper ⓘ Mt Riordan garnet deposit; Econ Geol () ⓘ Nickel Plate.Gold, Silver. Jowitt S M, Keays R R, Jackson P G, Hoggart C R and Green A H, - Mineralogical and Geochemical Controls on the Formation of the Woods Point Dike Swarm, Victoria, Australia: Evidence from the Morning Star Dike and Implications for Sourcing of Au Within Orogenic Gold Systems; in Econ.
Geol. v pp. Abia E H, Nachit H, Marignac C, Ibhi A, Saadi S A - The.