A recent Lithoprobe seismic-reflection transect in the Peace River arch region of the Western Canada sedimentary basin traverses continental crust that was...
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...
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...
Neoproterozoic strata of the southern Canadian Cordillera comprise metasedimentary rocks that are impressive in their thickness (6-9 km), areal extent (35,000...
The Proterozoic Muskwa assemblage is a thick (6 km) sequence of essentially unmetamorphosed, predominantly fine-grained siliciclastic and carbonate strata...
The Mesoproterozoic Belt-Purcell Supergroup is a thick succession of siliciclastic and carbonate sedimentary rocks in the northwestern United States and...
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...
Between 1992 and 1995, approximately 2000 km of seismic-reflection profiles were collected along three transects across the province of Alberta, as part of...
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