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1-20 OF 46 RESULTS FOR
Flatbed Creek
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A) Doe Creek allomembers 2 to 4 exposed in Flatbed Creek section 2 (arrows... Available to Purchase
in Allostratigraphy and paleogeography of the Upper Cenomanian, Lower Kaskapau Formation in subsurface and outcrop, Alberta and British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2006
Fig. 12. A) Doe Creek allomembers 2 to 4 exposed in Flatbed Creek section 2 (arrows indicate the top of each allomember). Note sharp-based, forced regressive delta-front sandstones in the upper parts of allomembers 2A, 3 and 4. The top of these sandstones are rooted and have dinosaur tracks
Image
A) Doe Creek allomembers 2 to 4 exposed in Flatbed Creek section 2 (arrows... Available to Purchase
in Allostratigraphy and paleogeography of the Upper Cenomanian, Lower Kaskapau Formation in subsurface and outcrop, Alberta and British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2006
Fig. 12. A) Doe Creek allomembers 2 to 4 exposed in Flatbed Creek section 2 (arrows indicate the top of each allomember). Note sharp-based, forced regressive delta-front sandstones in the upper parts of allomembers 2A, 3 and 4. The top of these sandstones are rooted and have dinosaur tracks
Image
Heterolithic facies B. A. Flatbed Creek, allomember 2A (site 7) showing cm-... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 9. Heterolithic facies B. A. Flatbed Creek, allomember 2A (site 7) showing cm-scale interstratified very fine-grained sandstone and siltstone with BI 0–1, sharply overlain by HCS sandstone of facies D. B. Heterolithic succession below shoreface sandstone. Heterolithic facies is incised
Image
A. 30 cm coal capping allomember AX5 in Flatbed Creek (see Fig. 11 ). Coal... Available to Purchase
in Anatomy of a late Cenomanian transgressive shelf system: The influence of high-frequency eustasy and crustal flexure on stratigraphy and paleogeography, basal Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2019
Figure 19. A. 30 cm coal capping allomember AX5 in Flatbed Creek (see Fig. 11 ). Coal is erosively overlain at transgressive surface X by a 1.2 m thick oyster biostrome that marks the base of the Doe Creek unit. B. Detail of mixture of attached and broken oyster shells, with an associated fauna
Image
Dip section line 2 extending from outcrop on Flatbed Creek, across the cent... Available to Purchase
in Allostratigraphy and paleogeography of the Upper Cenomanian, Lower Kaskapau Formation in subsurface and outcrop, Alberta and British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2006
Fig. 6. Dip section line 2 extending from outcrop on Flatbed Creek, across the central part of the basin to outcrop on the Peace River at Pratts Landing. Note eastward pinch-out of deltaic sandstones in the Doe Creek unit (allomembers 1–8) and reappearance of lowstand sandstones east
Image
Facies D. Stratified sandstone. A. Swaley and trough cross-stratified fine ... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 13. Facies D. Stratified sandstone. A. Swaley and trough cross-stratified fine sandstone, uppermost shoreface sandstone in allomember 2A at Flatbed Creek site 4, where it forms the ‘Lower Flatbed Falls’ of local terminology. B. Unit of large-scale trough cross-bedded sandstone locally
Image
Facies A, Thinly-bedded mudstone. A. Mudstone exposed near the base of allo... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 7. Facies A, Thinly-bedded mudstone. A. Mudstone exposed near the base of allomember 1 in Flatbed Creek; brown resistant bands comprise flattened siderite nodules (hammer = 32 cm long). B. Mudstone containing in-situ, vertically-oriented inoceramid bivalve (margin indicated by arrows
Image
Isolith maps for ‘clean’ (approximate
Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
cross-bedding; WR = wave ripple crest trend. Only allomember 1 contains an appreciable volume of sandstone, confined to the basin margin. Outcrop at Dickebusch Creek (DBC) and Flatbed Creek (FBC) shows that sandstones are thin (1–2 m) sharp-based shoreface deposits (see Figs. 10 , 12 ).
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Details of disarticulated shell beds forming reworked lags within facies A ... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Ostrea soleniscus Meek ( Stanton, 1893 ); D. Detail of internal surface of oyster shell showing encrusting serpulid worm tubes (coin = 18 mm diameter). Allomember A, Flatbed Creek.
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Isolith map of clean sandstone in AX3. Highstand sandstones are confined to... Available to Purchase
in Anatomy of a late Cenomanian transgressive shelf system: The influence of high-frequency eustasy and crustal flexure on stratigraphy and paleogeography, basal Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2019
Figure 26. Isolith map of clean sandstone in AX3. Highstand sandstones are confined to the NW, and wave ripples measured in Flatbed Creek indicate a shoreline trending NNE-SSW. A large elongate sandbody up to 7 m thick, interpreted as a wave-influenced lowstand shoreface, crops out at Torrens
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Figure 3. Cross section oriented SW-NE, transverse to axis of the basin (F... Available to Purchase
in Extensive thin sequences spanning Cretaceous foredeep suggest high-frequency eustatic control: Late Cenomanian, Western Canada foreland basin
> Geology
Published: 01 August 2007
Figure 3. Cross section oriented SW-NE, transverse to axis of the basin (Fig. 2) . Combined unconformity and/or flooding surfaces bounding sequences 1–6 in Flatbed Creek are correlated (on the basis of hundreds of well logs; details in Kreitner and Plint, 2006 ) to outcrop on distal side
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Heterolithic facies. A. Sandier-upward, heterolithic succession of facies B... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
. Longitudinal side view of a gutter cast in heterolithic facies showing HCS within the gutter fill; allomember 1, Flatbed Creek site 4. D. Exhumed gutter cast (loose, inverted; scale bar = 20 cm) showing rounded landward (NW) end and scratch and prod-marks on the gutter walls; Dickebusch Creek site 8. E. Large
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Generic summary of lateral facies relationships around the Doe Creek depoce... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 24. Generic summary of lateral facies relationships around the Doe Creek depocentre, with facies A through H indicated beside each log. Sections in Flatbed Creek in the far west show that 1–3 m thick shoreface/delta-front sandstones can pass laterally into nested gutter casts in 1–2 km
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Generalized paleogeographic reconstruction of the Doe Creek unit. The appro... Available to Purchase
in Allostratigraphy and paleogeography of the Upper Cenomanian, Lower Kaskapau Formation in subsurface and outcrop, Alberta and British Columbia
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2006
Highland Park to Erin Lodge, and in the west on Flatbed Creek indicate a broad embayment opening to the SE. The distribution of sandstone suggests the presence of rivers on the NW and SW margins of the embayment which fed deltas that prograded at highstand and falling stage to form extensive, sharp-based
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Facies D. Stratified sandstone. A. Overview of allomembers 1 and 1A in Flat... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 12. Facies D. Stratified sandstone. A. Overview of allomembers 1 and 1A in Flatbed Creek site 1. Marine deposits of allomember 1 are divided by a cryptic, rooted rubbly muddy paleosol. The location of images B to F are indicated by inset boxes. B. Thalassinoides network on the basal
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Correlation of the principal sections of Doe Creek allomembers 1 to 6 expos... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 6. Correlation of the principal sections of Doe Creek allomembers 1 to 6 exposed along Flatbed Creek, located a few kilometres south of the Tumbler Ridge town site (see inset map for location of the sections). The succession is gently folded such that the distinctive oyster biostrome above
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Mainly strike-oriented outcrop and core cross-section linking an offshore s... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 4. Mainly strike-oriented outcrop and core cross-section linking an offshore section at Nini Hill to basin-margin sections in Dickebusch Creek and Flatbed Creek (eight outcrop sections synthesized into two summary logs), then traced offshore via cores in the central part of the depocentre
Journal Article
High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin Available to Purchase
Publisher: Canadian Society of Petroleum Geologists
Published: 01 June 2019
Bulletin of Canadian Petroleum Geology (2019) 67 (2): 71–116.
...Figure 9. Heterolithic facies B. A. Flatbed Creek, allomember 2A (site 7) showing cm-scale interstratified very fine-grained sandstone and siltstone with BI 0–1, sharply overlain by HCS sandstone of facies D. B. Heterolithic succession below shoreface sandstone. Heterolithic facies is incised...
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Facies C, Bioturbated sandstone and mudstone. A. Dense network of Thalassin... Available to Purchase
in High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin
> Bulletin of Canadian Petroleum Geology
Published: 01 June 2019
Figure 11. Facies C, Bioturbated sandstone and mudstone. A. Dense network of Thalassinoides and ?Planolites on top surface of intensely bioturbated muddy sandstone package; Flatbed Creek site 2, allomember 5. B. Bioturbated muddy sandstone (BI 4–5) with remnants of original stratification. Trace
Journal Article
Extensive thin sequences spanning Cretaceous foredeep suggest high-frequency eustatic control: Late Cenomanian, Western Canada foreland basin Available to Purchase
Journal: Geology
Publisher: Geological Society of America
Published: 01 August 2007
Geology (2007) 35 (8): 735–738.
...Figure 3. Cross section oriented SW-NE, transverse to axis of the basin (Fig. 2) . Combined unconformity and/or flooding surfaces bounding sequences 1–6 in Flatbed Creek are correlated (on the basis of hundreds of well logs; details in Kreitner and Plint, 2006 ) to outcrop on distal side...
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