Muskwa Formation
| Muskwa Formation Stratigraphic range: Frasnian | |
|---|---|
| Type | Geological formation |
| Unit of | Horn River Formation |
| Underlies | Fort Simpson Formation |
| Overlies | Otter Park Member |
| Thickness | up to 34 metres (110 ft)[1] |
| Lithology | |
| Primary | Shale |
| Location | |
| Coordinates | 58°44′38″N 122°40′41″W / 58.7438°N 122.6781°WCoordinates: 58°44′38″N 122°40′41″W / 58.7438°N 122.6781°W |
| Region | British Columbia |
| Country |
 Canada |
| Type section | |
| Named for | Muskwa River |
| Named by | F.F. Gray and J.R. Kassube, 1963 |
The Muskwa Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.
It takes the name from Muskwa River, and was first described in the Western National Gas Fort Nelson a-95-J/94-J-10 well by F.F. Gray and J.R. Kassube, in 1963.
Lithology
The Muskwa Formation is composed of bituminous shale. Pyrite is a common accessory mineral.
Gas production
Gas is produced from the Muskwa Formation shales in the Horn River Basin in the Greater Sierra oil filed in north-eastern British Columbia. Horizontal drilling and fracturing techniques are used to extract the gas from the low permeability shales (see Shale gas).
Distribution
The Muskwa Formation occurs in northern Alberta, north-eastern British Columbia and in the southern part of the Northwest Territories, and typically has a thickness of 34 metres (110 ft).
Relationship to other units
The Muskwa Formation is a sub-unit of the Horn River Formation; it is conformably overlain by the Fort Simpson Formation and conformably underlain by the Otter Park Member.
See also
References
- ↑ Lexicon of Canadian Geological Units. "Muskwa Formation". Retrieved 2009-02-10.
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