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TitleStratigraphy and coal resource potential of the upper cretaceous to tertiary strata of northwestern Alberta
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AuthorDawson, F M; Kalkreuth, W D; Sweet, A R
SourceGeological Survey of Canada, Bulletin 466, 1994, 64 pages, https://doi.org/10.4095/194029
Year1994
PublisherNatural Resources Canada
Documentserial
Lang.English
MapsPublication contains 1 map
Map Info.geological, coal localities, 1:250,000
Mediapaper; on-line; digital
File formatpdf
ProvinceAlberta
NTS83D/09; 83D/10; 83D/11; 83D/12; 83D/13; 83D/14; 83D/15; 83D/16; 83E; 83L; 83M/01; 83M/02; 83M/03; 83M/04; 83M/05; 83M/06; 83M/07; 83M/08
AreaGrande Prairie; Smoky River; Wapiti River
Lat/Long WENS-120.0000 -118.0000 55.0000 53.5000
Subjectsstratigraphy; fossil fuels; sedimentology; Campanian; Paleocene; lithology; sandstones; siltstones; mudstones; coal; sedimentary rocks; depositional environment; coal ranks; coal seams; hydrocarbon potential; hydrocarbons; Upper Cretaceous; coal petrology; vitrinite reflectance; stratigraphic correlations; biostratigraphy; stratigraphic nomenclature; Coalspur Formation; Brazeau Formation; Scollard Formation; Paskapoo Formation; Tertiary; Cretaceous
Illustrationssketch maps; photographs; stratigraphic columns; analyses
Released1994 05 01; 2013 10 24
AbstractThe Late Campanian to Paleocene strata of northwest Alberta and northeast British Columbia consist of up to 1700 m of continentally derived sediments deposited in an eastward-thinning wedge. This thick sequence is contained within the Wapiti, Coalspur and Paskapoo formations. Lithologies consist of interbedded sandstone, siltstone and mudstone with minor coal, and appear to have been deposited in a predominantly fluvial environment. Three distinctive coal horizons þ Red Willow, Cutbank and Kakwa þ contain coal zones up to 8 m thick of subituminous to high-volatile A bituminous rank. These coals commonly contain numerous thin partings that may affect the mineability of the seams. Areas of exploration and development potential are highlighted for each of the coal measures.
GEOSCAN ID194029