Sm-Nd isotopic data are presented for 23 drill-core samples from five aeromagnetically and geochronologically (U-Pb zircon) distinct domains of the Precambrian...
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...
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...
Between 1992 and 1995, approximately 2000 km of seismic-reflection profiles were collected along three transects across the province of Alberta, as part of...
Neoproterozoic strata of the southern Canadian Cordillera comprise metasedimentary rocks that are impressive in their thickness (6-9 km), areal extent (35,000...
The Peace River Arch (PRA) is a roughly east-west striking cratonic element of the Western Canada Sedimentary Basin that cuts across the trend of underlying...
The Proterozoic Muskwa assemblage is a thick (6 km) sequence of essentially unmetamorphosed, predominantly fine-grained siliciclastic and carbonate strata...
Siliciclastic strata of Triassic age that are exposed in the Rocky Mountains have been sampled for isotopic studies in order to determine their provenance....
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