Elk Point Group | |
---|---|
Stratigraphic range: Early to Middle Devonian | |
Type | Geological formation |
Sub-units | Upper and Lower Elk Point Group |
Underlies | Beaverhill Lake Group, Manitoba Group |
Overlies | Precambrian to Silurian formations[1] |
Thickness | up to 610 metres (2,000 ft)[2] |
Lithology | |
Primary | dolomite, halite, anhydrite |
Other | Limestone, shale, potash |
Location | |
Coordinates | 53°54′19″N 110°37′49″W / 53.9053°N 110.6304°W |
Region | Northern plains |
Country | Canada United States |
Type section | |
Named for | Elk Point |
Named by | J.R. McGehee[3] |
The Elk Point Group is a stratigraphic unit of Early to Middle Devonian age in the Western Canada and Williston sedimentary basins. It underlies a large area that extends from the southern boundary of the Northwest Territories in Canada to North Dakota in the United States. It has been subdivided into numerous formations,[4] number of which host major petroleum and natural gas reservoirs.[5]
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