| Labiche Formation | |
|---|---|
| Stratigraphic range: late Albian to Santonian PreꞒ Ꞓ O S D C P T J K Pg N | |
| Type | Geological group |
| Underlies | Belly River Formation |
| Overlies | Pelican Formation |
| Thickness | up to 420 metres (1,380 ft) |
| Lithology | |
| Primary | Shale |
| Location | |
| Coordinates | 55°00′37″N 112°43′34″W / 55.01023°N 112.72600°W / 55.01023; -112.72600 (Labiche Formation) |
| Region | WCSB |
| Country |  Canada |
| Type section | |
| Named for | La Biche River |
| Named by | R.G. McConnell, 1892 |
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.
Lithology
The Labiche Formation is composed shale with flakes of coccolithic debris, Inoceramus prisms, pyrite.
Distribution
The Labiche Formation reaches a maximum thickness of 420 metres (1,380 ft) in the sub-surface of northern Alberta.
Relationship to other units
The Labiche Formation is overlain by the Belly River Formation and conformably overlays the Pelican Formation.
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
- ^ Lexicon of Canadian Geologic Units. "Labiche Formation". Retrieved 2010-01-09.
- 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.
| Western Canada Sedimentary Basin | |
|---|---|
| Hydrocarbon history | |
| Depositional regions |
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| Northeastern plains | |