Exshaw Formation

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Exshaw Formation
Stratigraphic range: Late Famennian to Middle Tournaisian
TypeGeological formation
Sub-unitsLower and Upper Exshaw
UnderliesBanff Formation
OverliesWabamun Formation, Kotcho Formation, Palliser Formation
Thicknessup to 50 metres (160 ft)[1]
Lithology
PrimaryShale
OtherSiltstone, limestone
Location
Coordinates51°05′29″N 115°09′29″W / 51.09139°N 115.15806°W / 51.09139; -115.15806 (Exshaw Formation)
RegionAlberta
CountryCanada
Type section
Named forExshaw, Alberta
Named byP.S. Warren, 1937[2]

The Exshaw Formation is a stratigraphic unit in the Western Canada Sedimentary Basin.[3] It takes the name from the hamlet of Exshaw, Alberta, in the Canadian Rockies, and was first described from outcrops on the banks of Jura Creek north of Exshaw by P.S. Warren in 1937.[2] The formation is of Late Devonian (late Famennian) to Early Mississippian (middle Tournaisian) age as determined by conodont biostratigraphy, and it straddles the DevonianCarboniferous boundary.[2][4]

The Exshaw strata were deposited in a marine setting during the Hangenberg event, an oceanic anoxic event associated with the Late Devonian extinction. The black shales of the Exshaw Formation are rich in organic matter and are one of the most important petroleum source rocks of the Western Canada Sedimentary Basin.[5]

The Exshaw Formation is informally subdivided into a lower shale member and an upper siltstone and limestone member. The lower shales are dark grey to black, thin-bedded to laminated, and rich in organic matter, with scattered sulphide and phosphate nodules.[1][6] There is no evidence of disturbance by biological activity. They are believed to have been deposited in an offshore environment on the outer continental shelf under anoxic conditions.[4][5] The shales are sparsely fossiliferous and contain some conodont elements, ostracods and brachiopod shells.[1][5]

The upper member consists of brown-weathering, medium- to thick-bedded, calcareous and dolomitic siltstones with subordinate silty limestones.[1][6] Bioturbation by burrowing marine organisms is common and indicates that they were deposited in an oxygenated environment, closer to the paleocoastline than the lower black shales were.[5]

Thickness and Distribution

Relationship to other units

References

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