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TitrePaskapoo groundwater study part VIII: Detailed core measured sections of the Paskapoo Formation in two cores at Sylvan Lake, Alberta
TéléchargerTéléchargements
AuteurHamblin, A P
SourceCommission géologique du Canada, Dossier public 6504, 2010, 9 pages, https://doi.org/10.4095/285363
Année2010
ÉditeurRessources naturelles Canada
Documentdossier public
Lang.anglais
DOIhttps://doi.org/10.4095/285363
Medianumérique; en ligne
Référence reliéeCette publication est reliée à les publications suivantes
Formatspdf
ProvinceAlberta
SNRC82J/16NE; 82O/01SE
Lat/Long OENS-114.2500 -114.0000 51.1333 50.7500
SujetsPaléogène; Paléocène; faciès sédimentaires; descriptions de faciès; structures sédimentaires; litage; discordances de ravinement; analyses stratigraphiques; roches sédimentaires; mudstones; silstones; grès; dépôts fluviaux; gîtes en forme de traînée; roches reservoirs; ressources en eau souterraine; aquifères; Formation de Paskapoo ; Membre de Dalehurst ; stratigraphie; hydrogéologie; Phanérozoïque; Cénozoïque; Tertiaire
Illustrationslocation maps; tables; stratigraphic sections
Consultation
Endroit
 
Bibliothèque de Ressources naturelles Canada - Ottawa (Sciences de la Terre)
 
ProgrammeAquifer Assessment & support to mapping, Géoscience des eaux souterraines
Diffusé2010 05 04
Résumé(disponible en anglais seulement)
The Paskapoo Formation, of Paleocene age, is an important, but poorly-understood groundwater aquifer in western Alberta, and is now emerging as a shallow gas reservoir. Because the Paskapoo represents the bedrock at surface over its area of occurrence, and has not previously been a major hydrocarbon target, there has been little study of outcrop or subsurface data. This report summarizes final subsurface core work in central Alberta, from two wells located at Sylvan Lake, which display strata from the upper portion of the Paskapoo. These latest two cores were cut during a recent joint project between Geological Survey of Canada and University of Calgary. In this report, the information is presented as standard measured sections, with text descriptions of units. The upper Paskapoo is characterized by thick, multi-storied fluvial channel sandstones and thinly interbedded siltstones and sandstones. This report is the final installment of basic stratigraphic/sedimentologic information on the Paskapoo, complementary to other Open Files (GSC OF 5392, 5445, 5535, 5536, 5537).
GEOSCAN ID285363