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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 ...