Coalspur Formation | |
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Stratigraphic range: | |
Type | Formation |
Unit of | Saunders Group |
Sub-units | Coalspur coal zone, Entrance conglomerate |
Underlies | Paskapoo Formation |
Overlies | Brazeau Formation |
Thickness | Up to about 550 metres (1,800 ft) |
Lithology | |
Primary | Sandstone, siltstone, shale |
Other | Coal, conglomerate, bentonite |
Location | |
Coordinates | 53°00′N 116°48′W / 53.0°N 116.8°W |
Approximate paleocoordinates | 60°36′N 91°36′W / 60.6°N 91.6°W |
Region | Alberta |
Country | Canada |
Extent | Western Canada Sedimentary Basin |
Type section | |
Named for | Coalspur, Alberta |
Named by | B.R. MacKay[1] |
Year defined | 1949 |
The Coalspur Formation is an Upper Cretaceous to lower Palaeocene stratigraphic unit of the Western Canada Sedimentary Basin in the foothills of southwestern Alberta.[2] Its deposition spanned the time interval from latest Cretaceous (Maastrichtian) to early Palaeocene, and it includes sediments that were deposited before, during, and after the Cretaceous-Paleogene (K-Pg) extinction event. It includes the economically important coal deposits of the Coalspur Coal Zone, as well as nonmarine plant and animal fossils.
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