The Precambrian crystalline basement of western Canada commonly is hypothesized to have been reactivated during the Phanerozoic and "basement control" is used...
Lithoprobe seismic-reflection profiles in the Western Canada Sedimentary Basin reveal a prominent band of dipping reflections that appear to extend into the...
The economy of northern Ontario, Canada is heavily dependent on mining, so accurate knowledge of seismicity is important for the safe design and operation of...
A recent Lithoprobe seismic-reflection transect in the Peace River arch region of the Western Canada sedimentary basin traverses continental crust that was...
Seismic migration and inversion are closely related processes for obtaining images of the subsurface. Both techniques attempt to infer petrophysical and...
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...
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...