Chloritoid-hornblende occurs in quartz-muscovite pelitic schist derived from sediment in a volcaniclastic sequence of the Grenville Supergroup and from...
A proposed correlation of major Archean shear zones across different metamorphic terranes of the central Superior province implies that the same shear zones...
Comparison of progressive deformation and metamorphic history within and between the tectonic domains of the Kapuskasing uplift indicates significant variation...
The northern edge of Phanerozoic platformal rocks of the Western Canada Sedimentary Basin overlies the Flin Flon Belt (Trans-Hudson Orogen) in Manitoba and...
The central Superior Province is transected by the intracratonic Kapuskasing uplift, which contains rocks exhumed from 30 to 35 km paleodepth. As part of the...