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La Biche Group

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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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