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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 ...
The Potential of microfossil use in paleodiet and paleoenvironmental analysis in Northwestern Ontario
(2008)
Historically wild rice was important economically and spiritually across much of central
and eastern Canada, but the antiquity of its use by Native communities is unclear. Unlike plant
macrofossils, which have traditionally ...
Paleomagnetic secular field variation and rock magnetism of some early holocene (<9900BP) postglacial lacustrine sediments near Thunder Bay, Northwestern Ontario, Canada
(2006)
Paleosecular magnetic changes through a 1.5m section of post-glacial lacustrine deposits
are strongly influenced by mineralogy and differential compaction. The sediments chiefly
comprise clay and, in the lower one third ...
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 ...
Magnetic fabrics of granitic plutons and gneisses, Northwestern Ontario
(2004)
Specimens of plutonic granitic gneisses have been collected from different
locations of the Superior Province. The study of their Koenigsberger ratio (related to
natural remanent magnetization) and the theoretical ...
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 ...
X-ray diffraction and Rietveld structural refinement of selected fluoroperovskites
(2000)
This study presents an X-ray diffraction analysis and Rietveld structural
refinement of selected synthetic fluoroperovskite-type compounds including the Na1-xKxMgF3 solid solution series in addition to synthetic analogues ...