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Author David J. Hughes in his 2004 book entitled North America's Natural Gas Crisis, predicted that the Western Canadian Sedimentary Basin would likely continue to be the main gas supply area in Canada for many years; however, declining production and the likelihood that much of the gas will be diverted to fuel new oil sands plants mean that ...
Montney Formation. The Montney Formation is a stratigraphical unit of Lower Triassic age in the Western Canadian Sedimentary Basin in British Columbia and Alberta.. It takes the name from the hamlet of Montney and was first described in Texaco's Buick Creek No. 7 well by J.H. Armitage in 1962. [3]
Western Canadian Sedimentary Basin Most of Canada's oil and gas production occurs in the Western Canadian Sedimentary Basin which stretches from southwestern Manitoba to northeastern BC. The basin also covers most of Alberta, the southern half of Saskatchewan and the southwest corner of the Northwest Territories .
The Viking Formation is conformably overlain by the Big River Formation and conformably and unconformably underlain by the Joli Fou Formation. [1]It is equivalent to the Bow Island Formation in southern Alberta, to the Newcastle Formation in North Dakota, to the Ashville Formation in Manitoba, the Pelican Sandstone in north-eastern Alberta and the Flotten Lake Sand in central Saskatchewan.
The Duvernay Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin. It was first described in well Anglo Canadian Beaverhill Lake No. 2 in LSD 11-11-50-17W4M by Imperial Oil staff in 1950. [2] The formation was named by Andrichuk and Wonfor in 1954 [3] for the type section in Duvernay, Alberta.
The Cardium Formation is a stratigraphic unit of Late Cretaceous age in the Western Canada Sedimentary Basin. It takes the name from the fossilized heart-shaped cockle shells in the family Cardiidae (from Greek καρδίᾱ kardiā, "heart") present. It was first described along the Bow River banks by James Hector in 1895. [2]
Natural gas is extracted from the Ostracod and Glauconite beds in southern Alberta, and light oil is extracted from the Ellerslie Member in central and southern Alberta. Multiple oil fields [3] and gas fields [4] tap into the Manville Group. Total gas reserves amount to 316 799 × 10 6 m 3 in the Lower Mannville and 644 774 × 10 6 m 3 in the ...
The Spirit River Formation is a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin. It takes the name from the Spirit River, and was first described in Imperial Oil Spirit River No. 1 well by Badgley in 1952. [2]