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TitleEvolution of the Judy Creek Complex, a late Middle Devonian isolate platform-reef complex in west-central Alberta
AuthorWendte, J C
SourceDevonian-Early Mississippian carbonates of the Western Canada Sedimentary Basin: a sequence stratigraphic framework; by Wendte, J; Stoakes, F A; Campbell, C V; SEPM (Society for Sedimentary Geology), Short Course no. 28, 1992 p. 89-125 (+ errata), https://doi.org/10.2110/scn.92.28.0089
Year1992
Alt SeriesEarth Sciences Sector, Contribution Series 20060536
PublisherSEPM (Society for Sedimentary Geology)
MeetingDevonian-Early Mississippian carbonates of the Western Canada Sedimentary Basin: a sequence stratigraphic framework: short course; Calgary, AB; CA; June 20-21, 1992
Documentserial
Lang.English
Mediapaper; on-line; digital
RelatedThis publication is contained in Wendte, J; Stoakes, F A; Campbell, C V; (1992). Devonian-Early Mississippian carbonates of the Western Canada Sedimentary Basin: a sequence stratigraphic framework, SEPM (Society for Sedimentary Geology), Short Course vol. 28
File formatpdf
ProvinceAlberta
NTS83J
AreaJudy Creek Complex
Lat/Long WENS-116.0000 -114.0000 55.0000 54.0000
Subjectsstratigraphy; sedimentary basins; sedimentary rocks; carbonates; basin evolution; sea level changes; tectonic history; tectonic setting; deposition; sedimentary facies; hydrocarbons; oil; gas; Western Canada Sedimentary Basin; Judy Creek Complex; stacking; hydrocarbon pools; Phanerozoic; Paleozoic; Devonian
Illustrationssketch maps; drawings; geological sketch maps; cross-sections, stratigraphic; photographs
AbstractReef complexes situated on carbonate platforms contain a disproportionate amount of hydrocarbon reserves. In Western Canada, approximately half of the oil and gas pools with recoverable reserves greater than 16 X 106 m3 (100 million barrels) of oil or its gas equivalent are Devonian reef complexes. Cores and wireline logs from producing and outlying wells from these pools provide perhaps an unparalleled opportunity to examine the evolution of reef complexes in all three dimensions. Most of the hydrocarbon bearing Devonian reef complexes in the WCSB are isolate features situated on areally widespread carbonate platforms. They include the Middle Devonian (late Givetian) Swan Hills reef complexes in west-central Alberta and the Kee Scarp buildup at Norman Wells in the Northwest Territories; and the Late Devonian (Frasnian) Leduc reef complexes in both east-central and west-central Alberta. The previous chapter dealt with the evolution of the underlying carbonate platform and its relationship to reef inception and localization. This chapter focuses primarily on the evolution of isolate platform-reef complexes. The Swan Hills buildup at Judy Creek in west-central Alberta is used as an example to illustrate the evolutionary development of these complexes.
GEOSCAN ID223248

 
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