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Depositional environments of the 3.0 Ga. Finlayson and Lumby Lake greenstone belts, Superior Province, Ontario, Canada
(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 ...
Paleomagnetism, structure and magnetic fabrics in a traverse of the Quetico subprovince between Atikokan and Kashabowie, NW Ontario
(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 ...
Rock magnetic and structural investigation of the Moss Lake stock and local area : western Shebandowan belt
(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 ...
An investigation of the use of anisotropy of complex magnetic susceptibility to analyse strain in experimentaly deformed materials and massive sulphides
(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 ...
Lithostratigraphy and provenance of the Neoarchean McKellar Harbour Sequence, Superior Province, Ontario, Canada
(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 ...
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
(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 ...
Petrography and mineralogy of the Lac de Gras kimberlite field, Slave Province, Northwest Territories : a comparative study
(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 ...
Stratigraphic architecture of a paleoproterozoic iron formation depositional system : the Gunflint, Mesabi and Cuyuna iron ranges
(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 ...
Silicate, sulfide, and platinum - group petrology and mineralogy of the Kawene Intrusion, Quetico subprovince
(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 ...
Neoarchean coastal sedimentation in the Shebandowan Group, Northwestern Ontario
(1996)
The study interpreted depositional environments from sedimentological data present
in metasedimentaiy rocks of the Neoarchean Shebandowan Group of the Wawa
Subprovince. Outcrops in the study area contained sedimentary ...