Assessment of undiscovered conventional oil and gas resources of the Western Canada Sedimentary Basin, Canada, 2012
The U.S. Geological Survey recently completed a geoscience-based assessment of undiscovered oil and gas resources of provinces within the Western Canada Sedimentary Basin. The Western Canada Sedimentary Basin primarily comprises the (1) Alberta Basin Province of Alberta, eastern British Columbia, and the southwestern Northwest Territories; (2) the Williston Basin Province of Saskatchewan, southeastern Alberta, and southern Manitoba; and (3) the Rocky Mountain Deformed Belt Province of western Alberta and eastern British Columbia. This report is part of the U.S. Geological Survey World Petroleum Resources Project assessment of priority geologic provinces of the world. The assessment was based on geoscience elements that define a total petroleum system (TPS) and associated assessment unit(s). These elements include petroleum source rocks (geochemical properties and petroleum generation, migration, and accumulation), reservoir description (reservoir presence, type, and quality), and petroleum traps (trap and seal types, and timing of trap and seal formation relative to petroleum migration). Using this framework, the Elk Point-Woodbend Composite TPS, Exshaw-Fernie-Mannville Composite TPS, and Middle through Upper Cretaceous Composite TPS were defined, and four conventional assessment units within the total petroleum systems were quantitatively assessed for undiscovered resources in the Western Canada Sedimentary Basin.
Citation Information
Publication Year | 2013 |
---|---|
Title | Assessment of undiscovered conventional oil and gas resources of the Western Canada Sedimentary Basin, Canada, 2012 |
DOI | 10.3133/fs20123148 |
Authors | Debra K. Higley |
Publication Type | Report |
Publication Subtype | USGS Numbered Series |
Series Title | Fact Sheet |
Series Number | 2012-3148 |
Index ID | fs20123148 |
Record Source | USGS Publications Warehouse |
USGS Organization | Central Energy Resources Science Center |