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Cooking Lake-Duvernay formations

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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1958
AAPG Bulletin (1958) 42 (9): 2189–2222.
... appears to be relatively abrupt, coincident with the bank margin. In the southeastern part of the map the Cooking Lake contains thin beds of anhydrite that increase in thickness and number toward the southeast. In general, the Duvernay formation consists of interbedded limestones and shales...
FIGURES | View All (15)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1961
AAPG Bulletin (1961) 45 (5): 612–632.
...John M. Andrichuk ABSTRACT In the Duhamel area of central Alberta, the Upper Devonian section under study comprises in ascending order: (1) Cooking Lake formation, (2) basal calcilutite of the Duvernay formation, (3) Leduc reef, and (4) Ireton formation. In off-reef sections, the Duvernay consists...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1958
AAPG Bulletin (1958) 42 (1): 1–93.
... is similar to that of the Perdrix formation of the exposed sections in the Alberta Rocky Mountains. In the dolomitized reef foundation area east of Leduc field, the Duvernay generally thins in response to carbonate buildup out of the underlying Cooking Lake unit. This may be observed in Okalta’s Leduc...
FIGURES | View All (35)
Journal Article
Published: 01 June 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (2): 164–185.
... Formation), reefal buildups (Leduc Formation) and basin-f i l l ing shales and l imestones (Majeau Lake Member, Ireton, Duvernay formations) (Fig. 2). Limestones and calcareous shales of the Waterways Formation (Beaverhill Lake Group, late Givetian and early Frasnian) underlie the Cooking Lake platform...
Image
—West-east cross section of <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> <b>formations</b> in souther...
Published: 01 September 1958
Fig. 3. —West-east cross section of Cooking Lake and Duvernay formations in southern part of area of study. Thin anhydrite beds and a biostrome occur in Cooking Lake at southeast. Widespread sparse bioclastic limestone is characteristic of basal Duvernay. Uppermost occurrence of brown to black
Image
—West-east cross section of <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> <b>formations</b> in Edmonto...
Published: 01 September 1958
Fig. 4. —West-east cross section of Cooking Lake and Duvernay formations in Edmonton area. Cooking Lake formation changes facies from bank limestones (calcarenites) east of Edmonton city, to secondary dolomites along Leduc-Morinville reef trend, and to basinal facies (argillaceous rocks
Image
—Northwest-southeast cross section of <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> <b>formations</b> ...
Published: 01 September 1958
Fig. 5. —Northwest-southeast cross section of Cooking Lake and Duvernay formations in northwestern part of map-area. Eastern part of dolomitized Cooking Lake foundation of Morinville reef of Leduc age shown in section K. In extreme northwestern part of area (north of bank margin), upper
Image
—West-east cross section of <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> <b>formations</b> in Willing...
Published: 01 September 1958
Fig. 8. —West-east cross section of Cooking Lake and Duvernay formations in Willingdon-Duvernay area. Biostromes present in Cooking Lake formation in all sections, and thickest in Duvernay area (section R). In section P, 950 feet of carbonates (Leduc reef) overlie the Cooking Lake formation.
Image
—Southwest-northeast cross section of <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> <b>formations</b> ...
Published: 01 September 1958
Fig. 10. —Southwest-northeast cross section of Cooking Lake and Duvernay formations in Sunland, Vilna, and Spedden areas. Two biostromes occur in Cooking Lake formation in section T (near north margin of interpreted Cooking Lake bank). Near Vilna and Spedden, north of bank margin, upper Cooking
Journal Article
Published: 01 December 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (4): 499–528.
...-central Alberta, deeper water basinal limestones of the Duvernay Formation overlie carbonates of the Cooking Lake Formation in off-reef positions. Overlying shales and argillaceous lime- stones of the Ireton Formation were coeval with and postdated Leduc reef development. SURFACE SUBSURFACE ARCS ~o...
Journal Article
Published: 01 March 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (1): 1–25.
... the time equivalent Cooking Lake Formation was deposited on the drowned Swan Hills platform. The overlying lower Leduc Formation shows backstepping and aggradational reef margin stacking patterns. Maximum relief from the carbonate platform to surrounding Duvernay Formation shale during the Upper...
Journal Article
Published: 01 December 1998
Bulletin of Canadian Petroleum Geology (1998) 46 (4): 515–563.
... Duvernay Formation extends into Zone 10. The Perdrix Formation in outcrop of the Rockies is largely equivalent in age to the Cooking Lake-Majeau Lake-Duvernay, but locally at least ranges into lower Zone 11. The black/grey shale facies of District of Mackenzie and northeast British Columbia (Canol...
Image
Schematic west-east cross section of <b>Cooking</b> <b>Lake</b>, <b>Duvernay</b>, and Leduc form...
Published: 01 May 1961
Fig. 13. Schematic west-east cross section of Cooking Lake, Duvernay, and Leduc formations showing major rocks deposited in reef and off-reef areas, Duhamel area, central Alberta.
Image
—South-north Leduc, <b>Cooking</b> <b>Lake</b>, <b>Duvernay</b>, and Ireton section across Stett...
Published: 01 January 1958
Fig. 18. —South-north Leduc, Cooking Lake, Duvernay, and Ireton section across Stettler and Erskine reefs. Lower limit of complete dolomitization in Leduc formation coincides with top of Cooking Lake formation in Stettler field and environs on north, whereas lower limit rises slightly north
Image
—North-south <b>Cooking</b> <b>Lake</b> and <b>Duvernay</b> cross section in off-reef area south...
Published: 01 January 1958
Fig. 19. —North-south Cooking Lake and Duvernay cross section in off-reef area southwest of Big Valley field. Lower limit of complete dolomitization in Gulf’s George 3 extends partly into Cooking Lake formation. This boundary rises in stratigraphic section eastward to Gulf’s Upton 1. “Brown
Journal Article
Journal: Geophysics
Published: 01 November 1989
Geophysics (1989) 54 (11): 1410–1419.
... on the Leduc-Woodbend atoll section; and reflections from the offreef shales (Duvernay and Ireton formations) terminate abruptly against the reef flank.In addition, the amplitude of the underlying Cooking Lake platform reflection varies laterally, depending on the velocity of the overlying formation (Duvernay...
Book Chapter

Author(s)
F.A. Stoakes
Series: SEPM Short Course Notes, SEPM Short Course Notes
Published: 01 January 1992
DOI: 10.2110/scn.92.28.0183
EISBN: 9781565762510
... Abstract This sequence comprises the strata between the Beaverhill Lake Group (Chapter 7) and the Winterburn Group (Chapter 9). The stratigraphic section includes shallow-water carbonates of the Cooking Lake, Leduc and Grosmont formations and deep-water carbonates and shales of the Majeau Lake...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1966
AAPG Bulletin (1966) 50 (3): 628.
... not yield conodonts; the Nisku contained a sparse fauna. In descending order, the Woodbend Group includes shale of the Ireton, limestone of the Duvernay, and limestone and dolomite of the Cooking Lake units. These last units are in juxtaposition with the reefs of the Leduc Formation. All Woodbend strata...
Journal Article
Published: 01 December 1990
Bulletin of Canadian Petroleum Geology (1990) 38 (4): 429–439.
.... Tentative comparisons are made with some Paleozoic algae; however, some of the Sturgeon Lake flora may be new species or genera. Preliminary examination of selected cores from the Ireton Formation and organic-rich Duvernay Formation in central Alberta indicates a widespread distribution of algal-derived...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1954
AAPG Bulletin (1954) 38 (12): 2500–2536.
... sections in the Edmonton area of central Alberta (Imperial Oil Limited Geological Staff, 1950). The Beaverhill Lake group in the Stettler area can be divided into five unnamed rock units. The Woodbend group is divisible into the Cooking Lake, Duvernay, Donalda, and Leahurst formations. The Winterburn...
FIGURES | View All (17)