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    AuthorAbdallah, Geoffrey Khalil (1)Craig, Susan Patricia (1)Dehls, John Fitzgerald (1)Farrell, Shannon Patrick (1)King, David (1)Koebernick, Christa Faith (1)Kowalski, Barbara Sylvia (1)Kukkee, Kenneth Robert (1)Lagroix, France (1)MacTavish, Allan Douglas (1)... View MoreSubjectGeology Ontario, Northwestern (3)Geomagnetism (3)Geology Ontario Lake Shebandowan Region (2)Intrusions (Geology) Ontario Atikokan Region (2)Mineralogy (2)Structural geology (2)Anisotropy (1)Apatite (1)Cathodoluminescence (1)Coldwell alkaline complex (1)... View MoreDate Issued1990 (5)1992 (3)1993 (3)1995 (3)1991 (2)1996 (2)1998 (2)1999 (2)1997 (1)xmlui.ArtifactBrowser.AdvancedSearch.type_discipline
    Geology (23)

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    Depositional environments of the 3.0 Ga. Finlayson and Lumby Lake greenstone belts, Superior Province, Ontario, Canada 

    King, David (1998)
    The Finlayson and Lumby Lake Greenstone BeHs are located approximately 200km west of Thunder Bay, Ontario, nom of Atikokan, Ontario. Within both the Finlayson Lake and Lumby Lake Grsenstom belts two distinct sequences ...
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    Paleomagnetism, structure and magnetic fabrics in a traverse of the Quetico subprovince between Atikokan and Kashabowie, NW Ontario 

    Werner, Tomasz (1993)
    The metasedimentary rocks along the traverse reveal low to high grade metamorphism from chlorite schist near Atikokan, through biotite schist to migmatites in the west within the centre of the Quetico Belt. Continuing ...
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    Rock magnetic and structural investigation of the Moss Lake stock and local area : western Shebandowan belt 

    Kukkee, Kenneth Robert (1995)
    The thesis area is located 120 km west of the City of Thunder Bay, Ontario, straddling the contact of the Quetico and Wawa subprovinces of the Archean Superior Province. Metasedimentary rocks of the Quetico Subprovince ...
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    Cathodoluminescence studies of feldspars and apatites from the Coldwell Alkaline Complex 

    Xiong, Jian (1995)
    The Coldwell alkaline Complex is located on the north shore of Lake Superior, and consists of three Centers representing three magmatic episodes. Center I consists of gabbro, and layered and unlayered ferroaugite syenite. ...
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    An investigation of the use of anisotropy of complex magnetic susceptibility to analyse strain in experimentaly deformed materials and massive sulphides 

    Puumala, Mark Allan (1991)
    Anisotropy of magnetic susce:ptibility (AivJS) has become a widely accepted method of fabric analysis in rocks, especially those which have been deformed tectonically. The use of anisotropy of complex magnetic suscepti ...
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    Lithostratigraphy and provenance of the Neoarchean McKellar Harbour Sequence, Superior Province, Ontario, Canada 

    Purdon, Robert Harrison (1995)
    The McKellar Harbour Sequence is located on the shore of Lake Superior approximately 40 km west of the town of Marathon, Ontario. The Sequence was examined in detail through stratigraphic and geochemical investigations ...
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    Geology, petrology, geochemistry and platinum-group element-gold-copper-nickel ore asselmblage [i.e. assemblage] of the Roby Zone, Lac Des Iles Mafic-Ultramafic Complex, Northwestern Ontario 

    Michaud, Michael Julien (1998)
    The Archean Lac des lies Complex is a mafic to ultramafic intrusion emplaced into gneissic tonalite. The Lac des lies Complex Is the largest of several mafic to ultramafic intrusions that form a circular outcrop pattern ...
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    Petrography and mineralogy of the Lac de Gras kimberlite field, Slave Province, Northwest Territories : a comparative study 

    Masun, Katharine Melanie (1999)
    The kimberlites studied from the Lac de Gras area are composed o f two broad textural types: hypabyssal kimberlite and volcaniclastic kimberlite. Hypabyssal kimberlite is present within small isolated dyke segments and ...
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    Stratigraphic architecture of a paleoproterozoic iron formation depositional system : the Gunflint, Mesabi and Cuyuna iron ranges 

    Pufahl, Peir Kenneth (1996)
    Understanding iron formation depositional processes has been hindered by the lack of precise modern analogues. However, by combining a regional basin analysis of sedimentary and volcanic rocks surrounding an iron formation ...
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    Silicate, sulfide, and platinum - group petrology and mineralogy of the Kawene Intrusion, Quetico subprovince 

    Selway, Julie Beryl (1993)
    The Kawene Intrusion is an ultramafic, layered, metamorphosed Cu- Ni- PGE- bearing intrusion located 29 km east of Atikokan within the Quetico Subprovince of northwestern Ontario. The Kawene Intrusion is emplaced primarily ...
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