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La Biche Group
From Wikipedia, the free encyclopedia
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The Labiche Formation is a stratigraphical unit of late Albian to Santonian age in the Western Canadian Sedimentary Basin.
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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]
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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
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