The Mesoproterozoic (1.47-1.40 Ga) Belt basin in western North America contains a thick succession of siliciclastic strata dominated by sediment derived from...
We address two problems of Cordilleran geology in this study using U-Pb dating of single detrital zircon grains from metasedimentary rocks: the provenance of...
A recent Lithoprobe seismic-reflection transect in the Peace River arch region of the Western Canada sedimentary basin traverses continental crust that was...
According to two recently proposed tectonic models for the accretionary history of the southern Canadian Cordillera, the Omineca Belt (the hinterland to the...
The Precambrian crystalline basement of western Canada commonly is hypothesized to have been reactivated during the Phanerozoic and "basement control" is used...
Sm-Nd isotopic data are presented for 23 drill-core samples from five aeromagnetically and geochronologically (U-Pb zircon) distinct domains of the Precambrian...
The western Canadian Shield of northern Alberta is composed of a series of continental slivers that were accreted to the margin of the Archean Rae hinterland...