Gravelbourg Formation

Coordinates: 49°27′50″N 108°35′34″W / 49.4638°N 108.5927°W / 49.4638; -108.5927 (Gravelbourg Formation)
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Gravelbourg Formation
Stratigraphic range: Bajocian
Type
Gravelbourg, Saskatchewan
Named byR.L. Milner and G.E. Thomas, 1954

The Gravelbourg Formation is a stratigraphical unit of Bajocian age in the Western Canadian Sedimentary Basin.

It takes the name from the town of

Gravelbourg, and was first described in well Tidewater Eastend Crown No. 1 by R.L. Milner and G.E. Thomas in 1954.[2]

Lithology

The Gravelbourg Formation is divided in two members, Lower and Upper Gravelbourg. The lower member is composed of

chalcedonic chert and anhydrite in the lower part and a basal shale bed with fish scales and anhydrite. The upper Gravelbourg consists of dark shale with sandstone and argillaceous limestone stringers and a tan mudstone
bed at the top. [1]

Distribution

The Gravelbourg Formation reaches a maximum thickness of 60 metres (200 ft) in the Williston Basin. At its type locality in southwestern Saskatchewan, it is 27 metres (90 ft) thick.[1] It thins out westwards at the eastern flank of the Sweetgrass Arch in southern Alberta and eastwards into southwestern Manitoba.

Relationship to other units

The Gravelbourg Formation is conformably overlain by the Shaunavon Formation. It conformably overlies the Watrous Formation in Manitoba and southeastern Saskatchewan, and unconformably overlays the Madison Group in south-eastern Alberta.[1]

The Lower Gravelbourg is equivalent to the

Piper Formation
in North Dakota and Montana.

References

  1. ^ a b c d Lexicon of Canadian Geologic Units. "Gravelbourg Formation". Retrieved 2010-01-31.
  2. ^ Milner, R.L. and Thomas, G E., 1954. Jurassic System in Saskatchewan. In: Western Canada Sedimentary Basin, American Association of Petroleum Geologists, p. 250-267