Reflection seismic data from the Colville Hills and Anderson Plain document an intracratonic compressional event, herein named the Forward orogeny, which...
Bovie Structure, which marks the eastern limit of Upper Cretaceous strata in the Liard Basin, is interpreted from seismic and well data to be a product of two...
Thick-skinned intracratonic structures reminiscent of those in the Rocky Mountain foreland of the United States are recorded in petroleum industry seismic data...
As a contribution to the Mackenzie Project of the Geological Survey of Canada's Geo-mapping for Energy and Minerals Program, bedrock mapping and stratigraphic...
The purpose of this cruise is to provide geological, sediment geodynamical, chemical and biological information required to evaluate any EIS related to the...
The Mackenzie Corridor, an area along the proposed route of the Mackenzie Valley pipeline, constitutes a significant petroleum frontier province in Canada's...
Knowledge of the deformation front of the Richardson Anticlinorium is an important component of assessments for regional hydrocarbon potential; but sparse...
A 320 km long, deep seismic reflection line across the central part of the Scotian Basin provides new insight on the deep stratigraphy of the basin, confirms...
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