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Scollard Formation

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Journal Article
Published: 01 March 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (1): 44–53.
...David A. Eberth; Shaun C. O’Connell ABSTRACT The Scollard Formation of southern Alberta comprises alluvial plain deposits that straddle the Cretaceous-Tertiary boundary. Paleochannels in the Scollard Formation display an apparent shift from low sinuosity (straight) to higher sinuosity (meandering...
Journal Article
Published: 25 January 2019
Canadian Journal of Earth Sciences (2019) 56 (10): 1041–1051.
... very low (∼1.40 cm/ka), and allows us to interpolate an age range of ∼66.88–67.20 Ma for the BFm. Our data also provide a maximum age of ∼66.88 Ma for the base of the overlying Scollard Formation, a dinosaur-rich unit. We combine our age data with calibrated magneto- and palynostratigraphic data...
FIGURES | View All (4)
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Stratigraphic relationships of Horseshoe Canyon and <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> spec...
Published: 15 December 2014
Fig. 1. Stratigraphic relationships of Horseshoe Canyon and Scollard Formation specimens of Edmontosaurus and chasmosaurine ceratopsians from southern Alberta. Derived from Eberth and Braman (2012) and Eberth et al. (2013) .
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Vertical profile for the Knudsen’s Farm locality, <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> (Maast...
Published: 01 September 2009
Fig. 4. Vertical profile for the Knudsen’s Farm locality, Scollard Formation (Maastrichtian and Paleocene). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop.
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Vertical profile for the Ardley locality, upper <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> (Paleoce...
Published: 01 September 2009
Fig. 6. Vertical profile for the Ardley locality, upper Scollard Formation (Paleocene). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop.
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Vertical profile for the Griffith’s Farm locality, lower <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span>...
Published: 01 September 2009
Fig. 7. Vertical profile for the Griffith’s Farm locality, lower Scollard Formation (Maastrichtian). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop.
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Vertical profile for the Kneehills Creek locality, lower <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span>...
Published: 01 September 2009
Fig. 8. Vertical profile for the Kneehills Creek locality, lower Scollard Formation (Maastrichtian). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop section.
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Vertical profile for the Hummer Hills locality, lower <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> (M...
Published: 01 September 2009
Fig. 9. Vertical profile for the Hummer Hills locality, lower Scollard Formation (Maastrichtian). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop section.
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Vertical profile for the Bow River locality, upper <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> (Pale...
Published: 01 September 2009
Fig. 10. Vertical profile for the Bow River locality, upper Scollard Formation (Paleocene). The table shows the sandstone composition in terms of relative percentages of the main authigenic clay minerals. Zero datum is the base of the outcrop section.
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Fig. 15.   (A) Outcrop of the Entrance Member (lower <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> – l...
Published: 12 June 2009
Fig. 15. (A) Outcrop of the Entrance Member (lower Scollard Formation – lower Coalspur Formation) along the Highway 40 South, Smoky River Valley ∼100 km south of Grande Prairie. B, lower beds of the Scollard–Coalspur formation near Grande Cache (Highway 40 South).
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Litho- and magnetostratigraphy of the <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span>. Cross-hatching in...
Published: 31 May 2007
Fig. 2. Litho- and magnetostratigraphy of the Scollard Formation. Cross-hatching indicates the stratigraphic interval exposed at Knudsen’s T . rex Ranch. After Eberth ( 2004 ). KTB, K–T boundary.
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Composite vertical profile of the <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> in the Red Deer Valley...
Published: 01 June 2004
Fig. 4. Composite vertical profile of the Scollard Formation in the Red Deer Valley region, showing the variability in lithofacies, framework constituents, and main authigenic mineral composition. Abbreviations: Q 1 – monocrystalline quartz; L 1 – lithoclasts (including polycrystalline quartz
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Classification of the <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> sandstones (after  Pettijohn et al...
Published: 01 March 2003
Fig. 10. Classification of the Scollard Formation sandstones (after Pettijohn et al., 1987 ).
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Composite vertical profiles of the <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> in the Red Deer Valle...
Published: 01 March 2003
Fig. 13. Composite vertical profiles of the Scollard Formation in the Red Deer Valley region, showing the variability in lithofacies (see Fig. 3 for symbols), framework constituents, and main authigenic mineral composition. Abbreviations: Q 1 – monocrystalline quartz; L 1 – lithoclasts
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Generalized diagenetic sequence for the <span class="search-highlight">Scollard</span> <span class="search-highlight">Formation</span> in the Red Deer ...
Published: 01 March 2003
Fig. 19. Generalized diagenetic sequence for the Scollard Formation in the Red Deer Valley region.
Journal Article
Published: 01 September 1985
Bulletin of Canadian Petroleum Geology (1985) 33 (3): 295–305.
...J.F. Lerbekmo; K.C. Coulter ABSTRACT Three partial sections of upper Horseshoe Canyon, Whitemud, Battle and Scollard formations at Horseshoe Canyon, Scollard Canyon and east of Wood Lake, in the southern, central and northern areas, respectively, of the Red Deer Valley were compared...
Journal Article
Published: 01 August 1983
Canadian Journal of Earth Sciences (1983) 20 (8): 1219–1231.
...Loris S. Russell Abstract The Scollard Formation is the uppermost division of the Edmonton Group in the Red Deer River valley of central Alberta. It dates from the close of Cretaceous and the beginning of Tertiary time. It rests on a very distinctive clay sequence consisting in descending order...
Journal Article
Published: 01 March 1995
Bulletin of Canadian Petroleum Geology (1995) 43 (1): 35–43.
... associées à la palynologie démontrent la présence des magnétozones 30, 29r et 29 dans le sud (formations Whitemud, Battle et Scollard), incluant le filon houiller qui marque la frontière Crétacé-Tertiaire mais non la “frontière argileuse”. Un grès de 23 m d’épaisseur qui devient brun lorsqu’il s’altère...
Journal Article
Published: 01 March 2003
Bulletin of Canadian Petroleum Geology (2003) 51 (1): 45–69.
...Fig. 10. Classification of the Scollard Formation sandstones (after Pettijohn et al., 1987 ). ...
FIGURES | View All (20)
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Fig. 4.   All illustrated material is stored in the permanent collection of...
Published: 15 September 2010
, slide b, N32/2. From basal Scollard Formation. (B) Aquilapollenites conatus Norton, 1965; TMP2008.204.0003; sample 3, slide b, H46/4. From basal Scollard Formation. (C) Aquilapollenites mtchedlishvili Srivastava, 1968; TMP2008.204.0004; sample 3, slide b, G30/3. From basal Scollard Formation. (D