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Fort St. John Group
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The Fort St. John Group is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin.[2] It takes the name from the city of Fort St. John, British Columbia and was first defined by George Mercer Dawson in 1881.

Key Information

Lithology

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The Fort St. John Group is mostly composed of dark shale deposited in a marine environment. Bentonite is present in the shale, and it is interbedded with sandstone, siltstone and conglomerates.

Distribution

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The Fort St. John Group occurs in the subsurface in the Peace River Country of northeastern British Columbia and north-western Alberta, in southern Yukon and southern Northwest Territories. It has a thickness of 700 metres (2,300 ft) to 2,000 metres (6,560 ft).

Relationship to other units

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The Fort St. John Group is conformably overlain by the Dunvegan Formation and conformably underlain by the Bullhead Group or may rest disconformably on older units.

Subdivisions

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The Fort St. John Group is subdivided into the following formations:

Sub-unit Age Lithology Max.
Thickness
Reference
Cruiser Formation Albian - Cenomanian marine shale, argillaceous siltstone and fine grained marine sandstone 230 m (750 ft) [3]
Goodrich Formation late Albian fine-grained, laminated sandstone, mudstone partings 400 m (1,310 ft) [4]
Hasler Formation middle to late Albian marine shale and siltstone, minor sandstone and pebble conglomerate 265 m (870 ft) [5]
Commotion Formation early to middle Albian sandstone, shale and conglomerate 490 m (1,610 ft) [6]
Gates Formation early Albian massive well-sorted sandstone, carbonaceous sandstone, mudstone, siltstone, coal 263 m (860 ft) [7]
Moosebar Formation early Albian marine shale and siltstone 289 m (950 ft) [8]
Sub-unit Age Lithology Max. Thickness Reference
Shaftesbury Formation Albian friable shale, fish scale siltstone, bentonite, ironstone 400 m (1,310 ft) [9]
Peace River Formation middle Albian Paddy Member - greywacke, coal
Cadotte Member - coarse to fine marine sandstone
Harmon Member - dark, fissile, non-calcareous shale
60 m (200 ft) [10]
Spirit River Formation middle Albian Notikewin Member - fine to medium grained argillaceous sandstone, dark shale, ironstone
Falher Member - greywacke, shale, siltstone, coal
Wilrich Member - dark shale thin sandstone and siltstone stringers
348 m (1,140 ft) [11]
Bluesky Formation early Albian brown, fine to medium grained, glauconitic, porous sandstone 46 m (150 ft) [12]
Sub-unit Age Lithology Max
Thickness
Reference
Sully Formation early to Late Cretaceous marine shale and siltstone 300 m (980 ft) [13]
Sikanni Formation early Cretaceous fine-grained, calcareous, glauconitic sandstone, argillaceous siltstone and shale 240 m (790 ft) [14]
Lepine Formation* middle to late Albian silty mudstone, sideritic concretions 900 m (2,950 ft) [15]
Scatter Formation* early to middle Albian Bulwell Member - glauconitic sandstone
Wildhorn Member - silty mudstone
Tussock Member - glauconitic sandstone, silty mudstone
375 m (1,230 ft) [16]
Garbutt Formation* early Aptian Lower Garbutt - mudstone, siltstone, siderite, bentonite
Upper Garbutt - mudstone, sideritic weathering, argillaceous siltstone, laminated sandstone
290 m (950 ft) [17]
Chinkeh Formation Barremian to early Albian sandstone with marine shale, conglomeratic base discontinuous [18]

*Buckinghorse Formation is equivalent to the sum of Lepine Formation, Scatter Formation and Garbutt Formation. It occurs north-east of the Canadian Rockies foothills in British Columbia, between the Halfway River and Muskwa River. It is composed of silty marine mudstone with fine grained marine sandstone interbeds.

References

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