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Kaskapau Formation

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Journal Article
Published: 01 June 2019
Bulletin of Canadian Petroleum Geology (2019) 67 (2): 71–116.
...A. Guy Plint; Michael A. Kreitner Abstract The great Late Cenomanian transgression of the Greenhorn Sea is recorded in western Alberta and adjacacent British Columbia by shallow-marine deposits of the lower Kaskapau Formation that blanket underlying deltaic deposits of the Dunvegan Formation...
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Journal Article
Published: 01 March 2019
Bulletin of Canadian Petroleum Geology (2019) 67 (1): 1–46.
...A. Guy Plint Abstract The late Cenomanian Kaskapau Formation records transgression of the Greenhorn Sea over deltaic strata of the Dunvegan Formation. However, stratigraphic and paleogeographic details of the initial stages of this profound reorganization of basin geography have not previously been...
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Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1198–1199.
... recent research that advocates looking for evidence of bedload transport of aggregated clays, and we are comfortable that much of the clay component in the Kaskapau Formation did indeed arrive via bedload transport rather than simply settling out of the water column. However, whereas we are perfectly...
Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1200–1201.
.... Plint A.G. MacQuaker J.H.S. Varban B.L. 2012 , Shallow-water, storm-influenced sedimentation on a distal, muddy ramp: Upper Cretaceous Kaskapau Formation, Western Canada Foreland Basin...
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Journal Article
Published: 01 November 2012
Journal of Sedimentary Research (2012) 82 (11): 801–822.
...A. Guy Plint; Joe H. S. Macquaker; Bogdan L. Varban Abstract: Mudstone-dominated shallow-marine rocks of the Kaskapau Formation were deposited on a low-gradient ramp that spanned the foredeep of the Western Canada foreland basin during the late Cenomanian to middle Turonian. Organic-, clay-rich...
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Series: SEPM Short Course Notes
Published: 01 January 2007
DOI: 10.2110/pec.07.52.0307
EISBN: 9781565761407
... on the Doe Creek Member of Kaskapau Formation. Zoophycos (Zo), Phycosiphon (Ph), Planolites (Pl), Scolicia (Sc), Palaeophycus (Pa), Thalassinoides (Th), Ophiomorpha (Op), Skolithos (Sk), Chondrites (Ch), Teichichnus (Te), Helminthopsis (He), Rhizocorallium (Rh), fugichnia (fu...
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Journal Article
Journal: PALAIOS
Published: 01 December 2006
PALAIOS (2006) 21 (6): 557–570.
...A. GUY PLINT; JISUO JIN; BOGDAN L. VARBAN; JESSICA R. RYLAARSDAM Abstract The Middle Turonian Kaskapau Formation in the Rocky Mountain Foothills of northeastern British Columbia comprises up to 950 m of shallow marine sandstones cyclically interstratified with marine mudstones and minor lagoonal...
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Journal Article
Published: 29 June 2006
Canadian Journal of Earth Sciences (2006) 43 (6): 631–652.
...Jessica R. Rylaarsdam; Bogdan L. Varban; A. Guy Plint; Lisa G. Buckley; Richard T. McCrea Abstract The Kaskapau Formation is a mudstone-dominated wedge up to 950 m thick that spans late Cenomanian to middle Turonian time. The formation has a prominent wedge geometry and was deposited...
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Journal Article
Published: 01 June 2006
Bulletin of Canadian Petroleum Geology (2006) 54 (2): 110–137.
...Michael A. Kreitner; A. Guy Plint Abstract The Kaskapau Formation is mudstone-dominated, ranges in age from Late Cenomanian to Middle Turonian, and records a phase of rapid flexural subsidence of the Western Canada foreland basin. The Late Cenomanian portion of the formation that lies above...
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Journal Article
Published: 01 December 2005
Bulletin of Canadian Petroleum Geology (2005) 53 (4): 357–389.
...Bogdan L. Varban; A. Guy Plint Abstract The Kaskapau Formation is a major, mudstone-dominated syntectonic wedge deposited in Late Cretaceous time in the foredeep of the Western Canada foreland basin. This study addresses the middle and upper parts of the formation (Late Cenomanian–Middle Turonian...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1993
AAPG Bulletin (1993) 77 (3): 414–435.
...Wallace-Dudley Karen; Leckie Dale ABSTRACT The Cenomanian to earliest Turonian (Cretaceous) Kaskapau Formation in northwestern Alberta and adjacent British Columbia contains three shallow-marine shelf sandstone bodies encased in shale: the Doe Creek, Pouce Coupe, and Howard Creek members...
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Journal Article
Published: 01 December 1989
Canadian Journal of Earth Sciences (1989) 26 (12): 2604–2620.
...Mark V. H. Wilson; Yael Chalifa Abstract Turonian fossil marine fishes occur at several localities near Watino, Alberta, in sandstones and in shale concretions of the Vimy Member, Kaskapau Formation. The actinopterygian fossils in the sandstone facies include Belonostomus , Ichthyodectes...
Journal Article
Published: 01 March 2000
Bulletin of Canadian Petroleum Geology (2000) 48 (1): 43–79.
... of the overlying Kaskapau Formation shows a 400 km shoreline backstep from Dunvegan allomember C, with the formation of a broad embayment fringed by low-energy, shoal-water deltas in the north. Coeval, wave-dominated sandbodies to the SE are isolated in shelf mudstone and might represent lowstand shoreline...
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Image
Regional study area of the <b>Kaskapau</b> <b>Formation</b> in NW Alberta and NE British ...
Published: 01 November 2012
Fig. 2 Regional study area of the Kaskapau Formation in NW Alberta and NE British Columbia showing distribution of well logs, core, and outcrops used by Varban (2004) to define the allostratigraphy of the formation. The location of the summary cross section in Figure 3 is shown. The Alberta
Image
Map showing the <b>Kaskapau</b> <b>Formation</b> outcrop belt, selected outcrop sections ...
Published: 01 June 2006
Fig. 5. Map showing the Kaskapau Formation outcrop belt, selected outcrop sections and location of wells used in the summary correlation lines 1 to 6, shown in Figures 6 to 11 . Map borders show Townships (N–S) and Ranges (E–W) of the Dominion Land Survey.
Image
Lithological partial sections of the <b>Kaskapau</b> <b>Formation</b> on Elephant and Tus...
Published: 11 December 2002
Fig. 2. Lithological partial sections of the Kaskapau Formation on Elephant and Tuskoola Mountains. Scale refers to vertical measurements only. Horizontal distance between the two outcrop sections is 4 to 5 km. Numbers (e.g., 39131) designate fossil collections made by the senior writer. G.S.C
Image
Correlation chart between surface outcrop section of the <b>Kaskapau</b> <b>Formation</b>...
Published: 11 December 2002
Fig. 3. Correlation chart between surface outcrop section of the Kaskapau Formation on Tuskoola Mountain (of Fig.  2 ) and the complete subsurface section of the Kaskapau Formation as drilled in the Phillips Puggins well ( Stott 1967 ). Bar scale refers to vertical measurement only. Horizontal
Image
Summary of facies in the lower <b>Kaskapau</b> <b>Formation</b>. Photographs are from uns...
Published: 01 March 1993
Fig. 5. Summary of facies in the lower Kaskapau Formation. Photographs are from unslabbed drill core. Each core is 9 cm (3.5 in.) wide. No photos for facies 9 and 10.
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 145–164.
Journal Article
Published: 01 December 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (4): 253–282.
... (then referred to by him as a formation) on a lithostratigraphic basis into three ‘members’: that is, “a lower shale [Kaskapau Formation], a middle sandstone — the ‘Bad Heart Sandstone’ [now a formation], and an upper shale [Puskwaskau Formation]”, with the type section for Bad Heart Formation being near...
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