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Burnt Timber Creek
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Foraminifera recovered from Burnt Timber Creek. (1) Lagenammina alexanderi...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
Fig. 7. Foraminifera recovered from Burnt Timber Creek. (1) Lagenammina alexanderi (Loeblich and Tappan). GSC 124236. (2) Reophax sikanniensis Stelck. GSC 124237. (3) Miliammina manitobensis Wickenden. GSC 124238. (4) Psamminopelta bowsheri Tappan. GSC 124239. (5) Ammobaculites
Journal Article
Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
Journal: Canadian Journal of Earth Sciences
Publisher: Canadian Science Publishing
Published: 31 July 2006
Canadian Journal of Earth Sciences (2007) 44 (7): 871–888.
...Fig. 7. Foraminifera recovered from Burnt Timber Creek. (1) Lagenammina alexanderi (Loeblich and Tappan). GSC 124236. (2) Reophax sikanniensis Stelck. GSC 124237. (3) Miliammina manitobensis Wickenden. GSC 124238. (4) Psamminopelta bowsheri Tappan. GSC 124239. (5) Ammobaculites...
Image
Dip line 3 links outcrop sections on Fallen Timber Creek, Burnt Timber Cree...
in Allostratigraphy of the Upper Cretaceous Cardium Formation in subsurface and outcrop in southern Alberta, and correlation to equivalent strata in northwestern Montana
> Bulletin of Canadian Petroleum Geology
Published: 01 March 2013
Figure 15 Dip line 3 links outcrop sections on Fallen Timber Creek, Burnt Timber Creek and Red Deer River to the subsurface grid. There is major erosion on E7, cutting down to the east, and surfaces E5.2 and E5.5 onlap westward onto E5. The presence of pebble or granule lags on these three
Image
(A) Map showing general location of the studied section on Burnt Timber Cre...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
Fig. 5. (A) Map showing general location of the studied section on Burnt Timber Creek. (B) Detailed location of Burnt Timber Creek section at National Topographic System (NTS) grid reference 82O/11 263111. Numbers on map border indicate NTS grid system.
Image
Series of representative outcrop sections through successive clinoform Dunv...
in Clinoforms, Paleobathymetry, and Mud Dispersal Across the Western Canada Cretaceous Foreland Basin: Evidence from the Cenomanian Dunvegan Formation and Contiguous Strata
> Journal of Sedimentary Research
Published: 01 March 2009
Figure 8 Series of representative outcrop sections through successive clinoform Dunvegan allomembers between Tea Creek in the NW and Burnt Timber Creek in the SE (located in Figure 1 ; correlation between Tea Creek outcrop and well 8-32-83-17W6, from which the FSU marker is picked, is shown
Image
A. Intensely bioturbated (B.I.=6) silty very fine sandstone in the upper pa...
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
); the sharp flooding surface is overlain by dark grey laminated mudstone at the base of AX4. C. The upper part of allomember AX3 at Burnt Timber Creek west consists of cm-scale, wave-rippled very fine-grained sandstone and siltstone interbeds that appear superficially well-stratified but in detail
Image
Combined outcrop and well log cross-section linking seven exposures of the ...
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 7. Combined outcrop and well log cross-section linking seven exposures of the A-X unit in the foothills between Smoky River (Twp 57) and Burnt Timber Creek (Twp 29). Facies are dominated by dark, thinly-bedded mudstone and siltstone, although the upper part of each allomember commonly
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Dip section 5–5′ showing interpreted correlation of Lower Colorado allogrou...
in An allostratigraphic correlation of Lower Colorado Group (Albian) and equivalent strata in Alberta and British Columbia, and Cenomanian rocks of the Upper Colorado Group in southern Alberta
> Bulletin of Canadian Petroleum Geology
Published: 01 December 2008
Fig. 15. Dip section 5–5′ showing interpreted correlation of Lower Colorado allogroup rocks into outcrop in two sections on Burnt Timber Creek. Joli Fou and Viking allomember boundaries are traced to major subaerial erosion surfaces or paleosols. Note westward onlap of Westgate unit WB onto VE4
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Summary paleogeography at sea-level lowstand. Well-sorted sandstones, shown...
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
exposed. The outlines of individual sandstone bodies in AX1 to AX5 are shown by broken coloured lines. The extent of the shoreline is speculative south of aapproximately 54°N, but is inferred to have at times protruded seaward in the vicinity of Ram River and Burnt Timber Creek, where allomember AX3
Image
Measured stratigraphic section through the Sunkay and basal Vimy members of...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
Fig. 6. Measured stratigraphic section through the Sunkay and basal Vimy members of the Blackstone Formation on Burnt Timber Creek. The base of the Blackstone Formation is marked by a thin chert pebble bed mantling rubbly terrestrial mudstones (paleosols) of the Blairmore Group. The lowest 1 m
Image
Schematic cross-sections, with approximate vertical and horizontal scales, ...
in An allostratigraphic framework for the Late Albian to Early Cenomanian upper Fort St. John Group across the foredeep of the Western Canada Foreland Basin, NE British Columbia
> Bulletin of Canadian Energy Geoscience
Published: 01 September 2022
, 36, 46 and 58 (based on Figures 15 to 18 in Roca et al., 2008 ). The cross-sections are correlated to outcrop sections in the fold and thrust belt, located on Burnt Timber Creek west, Ram River canyon, Brazeau River and Berland River, from south to north.
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Correlation line (located in Fig. 2 , based on 45 wells) extending across ...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
F1, Fig. 4. Correlation line (located in Fig. 2 , based on 45 wells) extending across Alberta from an outcrop section of the Sunkay and basal Vimy members of the Blackstone Formation on Burnt Timber Creek to Range 8W4. The logs are gamma ray and resistivity and the datum is the base of the Fish
Image
Northwest–southeast correlation line (located in Fig. 2 , based on 65 well...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
” surface mapped by Plint ( 2000 ) and commonly carries a veneer of small chert pebbles and granules. This pebble veneer can be traced southward to outcrop on Burnt Timber Creek (Fig. 3 ). The K1 surface is a major bevelling unconformity in the northwest, but becomes a disconformity in the study area
Image
Diagram summarizing the lateral stratigraphic relationships within the lowe...
in Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary
> Canadian Journal of Earth Sciences
Published: 31 July 2006
Fig. 1. Diagram summarizing the lateral stratigraphic relationships within the lower part of the Colorado Group. The SW side of the diagram represents a transect along the Alberta Foothills from the vicinity of Burnt Timber Creek (Tp. 30) northward to the vicinity of the Peace River
Journal Article
A relict triangle zone at Benjamin Creek gas field, southern Alberta foothills: geometry, kinematics and preservation
Publisher: Canadian Society of Petroleum Geologists
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 269–281.
...Roland G. Dechesne; James W. Muraro ABSTRACT A triangle zone with an internal duplex developed in Cretaceous Colorado Group strata occurs in the broad Williams Creek Syncline in the footwall of the Burnt Timber Thrust (Township 29, Range 7W5). The triangle zone fills the role of a footwall-ramp...
Journal Article
High-precision U–Pb zircon ID–TIMS dating of two regionally extensive bentonites: Cenomanian Stage, Western Canada Foreland Basin This article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh.
Journal: Canadian Journal of Earth Sciences
Publisher: Canadian Science Publishing
Published: 28 January 2011
Canadian Journal of Earth Sciences (2011) 48 (2): 543–556.
... precursor study to the results reported here is that of Tyagi et al. (2007) , who used physical sequence stratigraphy and foraminiferal biostratigraphy to link a well-exposed outcrop section on Burnt Timber Creek in the southern Alberta Foothills to a regional well log correlation grid established...
Journal Article
Stratigraphy and depositional history of the Burnt Timber Embayment, Fairholme Complex, Alberta
Publisher: Canadian Society of Petroleum Geologists
Published: 01 September 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (3): 290–306.
... Burnt Timber Creek (Twp 29, R 11 W5M; NTS map sheet 82 0/6 Lake Minnewanka) in the McConnell thrust sheet of the eastern Front Ranges (Fig. 2). The boundaries of the eight-km wide, shale-filled embayment are defined by the presence of carbonate buildup margins of the upper Cairn and Peechee members...
Journal Article
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
Publisher: Canadian Society of Petroleum Geologists
Published: 01 March 2019
Bulletin of Canadian Petroleum Geology (2019) 67 (1): 1–46.
...); the sharp flooding surface is overlain by dark grey laminated mudstone at the base of AX4. C. The upper part of allomember AX3 at Burnt Timber Creek west consists of cm-scale, wave-rippled very fine-grained sandstone and siltstone interbeds that appear superficially well-stratified but in detail...
Journal Article
Allostratigraphy of the Upper Cretaceous Cardium Formation in subsurface and outcrop in southern Alberta, and correlation to equivalent strata in northwestern Montana
Publisher: Canadian Society of Petroleum Geologists
Published: 01 March 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (1): 1–40.
...Figure 15 Dip line 3 links outcrop sections on Fallen Timber Creek, Burnt Timber Creek and Red Deer River to the subsurface grid. There is major erosion on E7, cutting down to the east, and surfaces E5.2 and E5.5 onlap westward onto E5. The presence of pebble or granule lags on these three...
Journal Article
Clinoforms, Paleobathymetry, and Mud Dispersal Across the Western Canada Cretaceous Foreland Basin: Evidence from the Cenomanian Dunvegan Formation and Contiguous Strata
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 March 2009
Journal of Sedimentary Research (2009) 79 (3): 144–161.
...Figure 8 Series of representative outcrop sections through successive clinoform Dunvegan allomembers between Tea Creek in the NW and Burnt Timber Creek in the SE (located in Figure 1 ; correlation between Tea Creek outcrop and well 8-32-83-17W6, from which the FSU marker is picked, is shown...
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