The Labiche Formation is a stratigraphical unit of late Albian to Santonian age in the Western Canadian Sedimentary Basin.

It takes the name from La Biche River, a tributary of the Athabasca River, and was first described in outcrop in the Athabasca River valley by R.G. McConnell in 1892.[2]

Lithology

The Labiche Formation is composed shale with flakes of coccolithic debris, Inoceramus prisms, pyrite.[1]

Distribution

The Labiche Formation reaches a maximum thickness of 420 metres (1,380 ft) in the sub-surface of northern Alberta.[1]

Relationship to other units

The Labiche Formation is overlain by the Belly River Formation and conformably overlays the Pelican Formation.[1]

It is equivalent to the parts of the Colorado Group in central Alberta and to the sum of Smoky Group, Dunvegan Formation and Shaftesbury Formation in north-western Alberta.

References

  1. ^ a b c d Lexicon of Canadian Geologic Units. "Labiche Formation". Retrieved 2010-01-09.
  2. ^ McConnell, R.G., 1893. Report on a portion of the district of Athabasca, comprising the country between Peace River and Athabasca River north of Lesser Slave Lake. Geological Survey of Canada, Annual Reptort (new series), 1890-91, v. 5, Part 1, p. 1-67.
Allikas: https://en.wikipedia.org/wiki/Labiche_Formation
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