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2 edition of petrography and mineralogy of the Cross Lake area, Ungava, New Quebec. found in the catalog.

petrography and mineralogy of the Cross Lake area, Ungava, New Quebec.

Norman Shepherd

petrography and mineralogy of the Cross Lake area, Ungava, New Quebec.

  • 143 Want to read
  • 15 Currently reading

Published in [Toronto] .
Written in English

    Subjects:
  • Mineralogy -- Quebec (Province) -- Cross Lake area,
  • Petrology -- Quebec (Province) -- Cross Lake area

  • Edition Notes

    ContributionsToronto, Ont. University.
    The Physical Object
    Paginationix, 176 leaves.
    Number of Pages176
    ID Numbers
    Open LibraryOL20173871M

      The Amisk Lake area contains an km thick sequence of subaerial and subaqueous flows and volcaniclastic rocks, including shallow water turbidites. The lower stratigraphy is dominated by transitional and tholeiitic basalt and basaltic andesite flows and volcaniclastic by: This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation. Volcanic stratigraphy, structural geology, and gold mineralization in the Wolverine-Doris corridor, northern Hope Bay volcanic belt, Nunavut lake felsic rocks show a gradation to more proximal phases to the north. There is good evidence for a Several felsic successions are recognized in the map area (Fig.2):theWolverine. Voisey's Bay Mine is a nickel mine in the Canadian province of Newfoundland and Labrador, near the bay of the same name. Latitude: 56° 20' " N Longitude: 62° 06' " W.

    crystalline rock in northern and eastern Canada and lake basins were gouged out from GEOL at Lone Star College System.


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petrography and mineralogy of the Cross Lake area, Ungava, New Quebec. by Norman Shepherd Download PDF EPUB FB2

Abstract. The U-Ni deposits at Key Lake, Sask., Canada, were presumably primarily formed under low-thermal near-palaeosurface conditions. The present genetical model is based on investigations of the geometry of the orebodies, weathering decomposition of basement rocks (source) with anomalously high U and Ni clarke values and local synmetamorphic U and Ni mineral enrichments, ore textures and Cited by: 4.

Pegmatite Mineralogy: Cross Lake, Manitoba. Richard Gunter Cedarcreek Drive Chilliwack, British Columbia, Canada V2R 5K4 [email protected] Abstract: The New Quebec. book Lake Pegmatite Field is a complex system of four pegmatite suites.

Two of the suites; the Northern Series. Geochemistry and petrology of the Loon Lake pluton, Ontario [microform] / West to east emplacement ages along a northern and southern cross-section of this belt range from Ma (Kensington Author: Jaroslav Dostal.

In book: Field Guidebook for the 87th Annual Meeting of the New York State Geological Association, SUNY Plattsburgh, September 12Chapter: GEOLOGY AND PETROLOGY OF THE MONT ROYAL Author: Nelson Eby. The geology and petrography of Mount Yamaska, province of Quebec [electronic resource] / (Ottawa: S.E.

Dawson, ), by G. Young and Geological Survey of Canada (page images at HathiTrust) The Archæan geology of Rainy Lake re-studied [electronic resource] / (Ottawa: Govt. Print. Three types of subvertical pegmatitic leucogranites and pegmatites populate the Red Cross Lake pegmatite field, located in a greenstone belt of the Sachigo Subprovince, Manitoba, in the northwestern part of the Archean Superior Province of the Canadian by: GEOLOGY AND PHYSIOGRAPHY OF THE LAKE SAINT-JEAN AREA 83 PHOTO I (R.C.A.F.

Photo AS) The Shield-Iowland contact at the western edge of the Lake Saint-Jean basin. Hère the contact is rectilinear and abrupt. It is bordered on the lowland side by fiuvioglacial deposits and a string of kettle-form Iakes.

Physiography and Glacial Geology of Gaspe Peninsula, Quebec (Bulletin No. 34) [Coleman, A.P.] on *FREE* shipping on qualifying offers. Physiography and Glacial Geology of Gaspe Peninsula, Quebec (Bulletin No. 34)Author: A.P. New Quebec. book. Geology and Mineral Deposits of Ville-Marie and Guillet (Mud) Lake Map- Areas, Quebecq [Henderson, J.F.] on *FREE* shipping on qualifying offers.

Geology and Mineral Deposits of Ville-Marie and Guillet (Mud) Lake Map- Areas, QuebecqAuthor: J.F. Henderson. The Ashton–SOQUEM joint venture entered into the Quebec portion of the Superior Craton inafter desktop and field studies concluded that the area was prospective for diamonds.

A collection of widely spaced samples of Quaternary deposits coveringkm 2 defined several anomalies, based on small counts of mantle indicator Cited by: wholeformofthemainlake,andthepositionsoftheinlet and outlet, present a strikingresemblance tothe outline of the humanstomach andthe situations ofits orifices".Island.

ore petrology and. wallrock alteration studies. at the. lake shore gold mine, kirkland lake, ontario. brent ian mcinnes. a thesis submitted as partial fulfillment for the honours bachelor of science degree.

faculty of science mcmaster university hamilton, ontario. april, Author: Brent Ian McInnes. Moonshine Mine, Lardeau Area, British Columbia; Mineralogy Richard Gunter Cedarcreek Drive Chilliwack, British Columbia [email protected] Abstract: The Moonshine Mine is a small, intermittently mined lead-silver deposit in the Kootenay Area of eastern British Columbia.

Clowes, Ronald Wyman, Derek and Kerrich, Robert Mantle plume – volcanic arc interaction: consequences for magmatism, metallogeny, and cratonization in the Abitibi and Wawa subprovinces, CanadaThis article is one of a series of papers published in this Special Issue on the theme Lithoprobe — parameters, processes, and the evolution of a by: New mining camp in the Baie James region.

Since the discovery of the world-class Roberto gold deposit, the Baie James region has experienced a major boom in mineral exploration. Several mineral occurrences have been discovered in a variety of metallogenic settings.

Moreover, this area is much larger and less well known compared to the Abitibi. Close mobile search navigation. Article navigation. Vol Number 1Cited by: these deltaic systems, with emphasis on mineralogy, res - ervoir quality, provenance, and petroleum potential, was conducted by Bartsch-Winkler (, ), Bartsch-Win-kler and Huffman (), and Johnsson and Sokol ().

Reservoir quality of the Nanushuk sandstones was previ - ously investigated by Reifenstuhl and Loveland (). TheFile Size: 3MB. The study area lies along a radiometrically anomalous migmatite belt situated within the Beren's River Block of the Superior Province, northwestern Ontario.

This belt trends roughly S-SE between Favourable Lake and Bearhead Lake (see MapFavourable Lake - Beren's Lake Sheet, Geological Compilation Series, Ayres, : Randall T.

Gillespie. From Small Beginnings Come Great Things: Correlating Mineralogy from Thin-Sections to Production History for the Panther River Tight Gas Field, Alberta, Canada* Chad Glemser1 and Jeffrey MacDonald2 Search and Discovery Article # () Posted Febru   Welcome to our web site.

Below you may find River in Quebec, Canada, that flows into the St Lawrence River near Sept-Iles crossword clue answers Mirror Quiz Crossword Puzzle.

You are here because you are looking for the answer of River in Quebec, Canada, that flows into the St Lawrence River near Sept-Iles crossword. Published by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume This guidebook was prepared for field trip T, "Early Proterozoic Rocks of the Great Lakes Region," as part of the 28th International Geological Congress in Washington, D.C., July LibraryThing Review User Review - shoomg - LibraryThing.

This is an interesting and informative book about the geology, fossils, and landforms on Manitoulin Island, the largest freshwater island in the world, located at the northern end of Lake Huron in 5/5(1).

Petrology of the Renard igneous bodies: host rocks for diamond in the northern Otish Mountains region, Quebec T.C. Birkett a, *, T.E. McCandless b, C.T. Hood b aSOQUEM INC., route de Eglise, Sainte-Foy, Quebec, Canada G1V 3V9 bAshton Mining of Canada Inc., Unit West 1st Street, North Vancouver, BC, Canada V7P 3N4 Received 21 June ; accepted 4 January   The Chibougamau mining camp, a major gold producer, has so far produced a total of 1, mt of gold at an average grade of g/tonne.

In contrast to a general tendency to group the deposits as vein type with varying compositions, this paper demonstrates the strong influence of regional lithologic and tectonic evolution of the area on the gold mineralization by: Try the new Google Books Get print book.

No eBook available across web, tablet, and phone. Go to Google Play Now» Glacial geology of the Laurentian Divide area, St. Louis and Lake Counties, Minnesota: J.D. Lehr and Howard C.

Hobbs, leaders. From inside the book. What people are saying - Write a review. We haven't found any reviews in. THE HARP LAKE COMPLEX, LABRADOR, AND THE MORIN COMPLEX, QUEBEC HARP LAKE COMPLEX AN Feldspars mol percent CA MG CA FE I a b Pyroxenes and Fe olivines MG FE cat ion percent Fig.

- a) Analyzed feldspars of the Harp Lake complex. b) Analyzed pyroxenes and Fe-rich olivines from the Harp Lake complex. Fe is total by: 4. CALIFORNIA JOURNAL OF MINES AND GEOLOGY, JANUARY ; VOL NUMBER 1 and a great selection of related books, art and collectibles available now at   At approximately 16 ha (~41 acres) in surface area, Grand Lake is the largest inland lake in New Brunswick and in all of Atlantic Canada.

The lake connects with the Saint John River via the Jemseg River, approximately km in length (Fig. 2). From Small Beginnings Come Great Things: Correlating Mineralogy from Thin-sections to Production History for the Panther River Tight Gas Field, Alberta, Canada.

Chad Glemser1 and Jeffrey MacDonald2. 1Shell Canada Limited, Calgary, Alberta, Canada. 2Osum Oil Sands Corp., Calgary, Alberta, Canada. The Lake Alma Member consists of laminated dolomudstones overlain by bedded to nodular anhydrite reflecting a increasingly hypersaline shallow subtidal environment.

The Coronach Member has burrowed skeletal wackestones at the base, laminated dolomite in the middle, and, in the basin centre, bedded anhydrite at the top. a,b,c), this paper focuses on the petrography and geochemistry of fine- and medium-crystalline dolomites, and compares them with late-stage coarse-crystalline and saddle dolomites.

GEOLOGICAL SETTING The Middle Devonian Presqu’ile barrier is located in the northern part of the Western Canada Sedimentary Basin (Fig. It is a linear. Considerations relating to the Quebec group and the upper copper-bearing rocks of Lake Superior (Canadian Natu- ralist vol.

vi, pp.May ) ; with a vertical section extending from Montmorency to the Island of Orleans, p. ; and a diagram at p.showing the author's opinion on the deposit of the Potsdam, Quebec group, Birdseye.

Lake Havasu Agate 58 Dendritic White Opalite at Goffs 61 Danby Opalite and Agate 63 Fossil Trilobites and Marble at Cadiz 65 Marble Mountains Garnet and Hematite 67 Kelbaker Road Nodules and Chalcedony 69 Providence Mountains Iron Minerals 71 Old Camp Carnelian and Chalcedony Roses 73 Ludlow Gems 75 illFile Size: KB.

A petrographic study of the Metamorphic rocks of the Chisel lake area, northern Manitoba. Williams, Harold imprint [] description. 1 v. format(s) Thesis Back; 0 Marked; Mark; A petrographic study of the Metamorphic rocks of the Chisel lake area, northern Manitoba.

series title. Theses, Ph.D., imprint [] dissertation note. GEOSCAN RSS feed for GEM2: Geo-mapping for Energy and Minerals publications40Ar/39Ar hornblende and biotite cooling ages for metaplutonic rocks of the central Thelon Tectonic Zone, Nunavut.

AREA Background Information Introduction Wawa is located km north of Sault Ste. Marie, Ontario, east of Lake Superior (Figure 1). Wawa, accessed by High Highway or scheduled air service, sits on the Michipicoten greenstone belt which has been mined for iron and gold since (Gledhill ) History of Quaternary Geology Mapping File Size: 1MB.

Most reconstructions of the final phase of Lake Ojibway depict the lake coalesced with glacial Lake Agassiz and inundating the entire Hudson Bay lowlands from Manitoba to Quebec (e.g. Leverington et al.,Clarke et al.,Dyke, ).A shared water plane with Lake Agassiz should have occurred after ice retreat from the Agutua-Nakina moraine in northern by: J.

McDivitt, Kontak, D. J., Lafrance, B., and Robichaud, L., “ Contrasting fluid chemistries, alteration characteristics, and metamorphic timing relationships recorded in hybridized orebodies of the Missanabie-Renabie gold district, Archean Wawa Subprovince, Ontario, Canada ”, Economic Geology and the Bulletin of the Society of Economic GeologistsEconomic Geology and the Bulletin of the.

This study marks the third consecutive regional investigation of mineralization associated with rare-element pegmatites and related S-type, peraluminous granites in the Superior Province of Ontario. Although the Georgia Lake pegmatite field within the Quetico Subprovince has witnessed a long period of exploration for various rare-elements and most notably lithium since its discovery in the mid.

WONES: LUCERNE PLUTON 4t5 Geology of the Lucerne pluton The intrusive nature of the Lucerne pluton can be observed in a variety of locations (Wones,) (Fig. In North Penobscot, Maine, an apo-physis of the pluton, m wide, exploits a pre-existing fault zone between the Penobscot Formation and the South Penobscot pluton.

Discover the best homework help resource for GEOLOGY at Laurentian University. Find GEOLOGY study guides, notes, and practice tests for Laurentian University.2D geological model of the Becancour area between Montreal and Quebec City.

The simulation results show that the likelihood of reactivating two reservoir-bounding faults (Yamaska and Champlain Faults) strongly depends on reservoir pressure at the faults, which in turn depends on.A new interpretation of the Katinik nickel deposit, Ungava, northern Quebec.

Economic Geol Barnes S.-J. and Giovenazzo D., Platinum-group elements in the Bravo Intrusion, Cape Smith Fold Belt, Northern Quebec. Canadian Mineralog Barnes S.-J. and Often M., Ti-rich komatiites from northern Norway.