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- W2134136093 abstract "The Three Forks Group includes the Torquay, Big Valley and Bakken Formations in Saskatchewan (Christopher, 1961) and are latest Devonian (Famennian) and earliest Mississippian (Kinderhookian) in age. The two cores on display are east of the Big Valley depositional edge and hence have Bakken deposited directly on Torquay. The Big Valley Formation rests unconformably on Torquay regionally, but there is little evidence of significant erosion on this surface. The Big Valley represents the third Famennian transgression according to Sandberg, et al (1988). Christopher (1961) subdivided the Torquay Formation into six units which he correlated across southern Saskatchewan (Units 1-6). The cores display a sequence boundary at the top of Unit 3; the lower three Units (Unit 1-3) are shallow lagoon and debris flow beds with a distinctive red iron oxide colour. The base of Unit 4 represents a transgressive flooding surface with Lower Shoreface sands deposited directly on red bed debris flow sediments. The upper Units (Units 4-6) are not altered by oxidation in the display core. The uppermost Unit has a soil profile (Unit 6)." @default.
- W2134136093 created "2016-06-24" @default.
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- W2134136093 date "1999-01-01" @default.
- W2134136093 modified "2023-09-27" @default.
- W2134136093 title "The Three Forks Group (Upper Devonian and Lower Mississippian) of the Williston Basin, southeast Saskatchewan" @default.
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