Keg River Formation

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Keg River Formation
Stratigraphic range: Givetian
TypeGeological formation
UnderliesMuskeg Formation
OverliesChinchaga Formation
Thicknessup to 300 metres (980 ft)[1]
Lithology
PrimaryDolomite, limestone
Location
Coordinates59°10′21″N 118°44′54″W / 59.1725°N 118.7482°W / 59.1725; -118.7482 (Keg River Formation)Coordinates: 59°10′21″N 118°44′54″W / 59.1725°N 118.7482°W / 59.1725; -118.7482 (Keg River Formation)
Region Alberta
Country Canada
Type section
Named for
Named byJ. Law
Year defined1955

The Keg River Formation is a stratigraphic unit of Givetian age in the Western Canada Sedimentary Basin.

Description[]

It takes the name from the Keg River, a tributary of the Peace River, and was first described in the California Standard Steen River 2-22-117-5W6M well (situated north of Zama Lake) by J. Law in 1955.

Lithology[]

The Keg River Formation is composed of dark dolomite with intercrystalline or vuggy porosity and wackestone limestone. [1] The Rainbow Member and upper Keg River Member are reef formations deposited in the Rainbow, Zama and Bitscho sub-basins.

Distribution[]

The Keg River Formation occurs in the subsurface from northeastern to northwestern Alberta and its southern border is defined by the . It varies in depth from 10 metres (30 ft) to 300 metres (980 ft).[1]

Relationship to other units[]

The Keg River Formation is conformably overlain by the Muskeg Formation and unconformably overlays the Chinchaga Formation.[1]

It is equivalent to the Pine Point Formation, Hume Formation and Nahanni Formation in north-eastern British Columbia and the Northwest Territories and to the Winnipegosis Formation in Saskatchewan and eastern Alberta.

Economic geology[]

Petroleum geology[]

Oil is produced from the Keg River reefs in the Zama Lake and Rainbow Lake areas of north-western Alberta.

References[]

  1. ^ a b c d Lexicon of Canadian Geologic Units. "Keg River Formation". Archived from the original on 2009-04-16. Retrieved 2009-03-01.
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