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Belloy Formation

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Named by
  
H.L. Halbertsma, 1959

Primary
  
Overlies
  
Country
  
Province
  
Named for
  
Thickness
  
up to 274 metres (900 ft)

Other
  
Region
  
Alberta,  British Columbia

Underlies
  

The Belloy Formation is a stratigraphical unit of Permian age in the Western Canadian Sedimentary Basin.

Contents

It takes the name from the hamlet of Belloy, Alberta, and was first described in the Imperial Belloy 12-14-78-1W6M well by H.L. Halbertsma in 1959.

Lithology and Depositional Setting

The Belloy Formation is composed of mixed carbonate-siliciclastic sequences of cherty dolostone and sandstone, glauconitic and quartz sandstones, phosphorite, siltstones and conglomerate with phosphatic chert pebbles. The Belloy was deposited along a northwest-trending, tidally-influenced, west-prograding shoreline.

Distribution

The Belloy Formation reaches a maximum thickness of 274 metres (900 ft) in the Canadian Rockies foothills south of Fort St. John. It thins out towards the east and occurs in the sub-surface throughout the Peace River Country.

Relationship to other units

The Belloy Formation is disconformably overlain by Triassic or younger beds (Montney Formation, Fort St. John Group). It is unconformably overlies Mississippian sediments such as those of the Rundle Group.

The Bellow Formation is homotaxial with the Belcourt Formation and Kindle Formation of the Rocky Mountains.

References

Belloy Formation Wikipedia


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