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040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-ab
0861 |aM183-2/8903E-PDF
1001 |aArdakani, O. H., |eauthor.
24510|aOrganic petrography and thermal maturity of the Paskapoo Formation in the Fox Creek area, west-central Alberta / |cO.H. Ardakani.
264 1|a[Ottawa] : |bGeological Survey of Canada, |c2022.
264 4|c©2022
300 |a1 online resource (20 pages) : |billustrations (chiefly colour), colour map.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aOpen file, |x2816-7155 ; |v8903
504 |aIncludes bibliographical references (pages 18-20).
5203 |a"The Paskapoo Formation, which ranges in age from middle to upper Paleocene, is the major shallow aquifer in Alberta. This study is part of a larger GSC-led study on the potential environmental impact of hydrocarbon development in the Fox Creek area (west-central Alberta) on shallow aquifers. Fox Creekis located near the northern limit of the Paskapoo Formation. In addition to the underlying organic-rich source rocks in the study area, including the Duvernay Formation that is currently exploited for hydrocarbon resources, the Paskapoo Formation contains organic-rich intervals and coal seams. In order to investigate any potential internal hydrocarbon sources within the Paskapoo Formation, ninety-seven (97) cutting samples from the formation obtained from eight shallow monitoring wells (50-90 m) in the study area were studied for total organic carbon (TOC) content, organic matter composition and thermal maturity of coal seams using programmed pyrolysis analysis and organic petrography"--Abstract, page 2.
650 0|aPetroleum|xGeology|zAlberta.
650 0|aPetrology|zAlberta.
650 0|aPyrolysis.
650 6|aPétrole|xGéologie|zAlberta.
650 6|aPétrologie|zAlberta.
650 6|aPyrolyse.
7102 |aGeological Survey of Canada, |eissuing body.
830#0|aOpen file (Geological Survey of Canada)|v8903.|w(CaOODSP)9.506878
85640|qPDF|s20.18 MB|uhttps://publications.gc.ca/collections/collection_2022/rncan-nrcan/m183-2/M183-2-8903-eng.pdf
8564 |qHTML|sN/A|uhttps://doi.org/10.4095/330296