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Journal Article

Stratigraphy of the Bad Heart Formation, Clear Hills and Smoky River areas, Alberta Available to Purchase

B. Kafle, R.A. Olson, O. Catuneanu
Published: 01 December 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (4): 253–282.
DOI: https://doi.org/10.2113/gscpgbull.61.4.253
...B. Kafle; R.A. Olson; O. Catuneanu Abstract The Upper Cretaceous (mid to late Coniacian) Bad Heart Formation consists of a ‘coarser’ clastic succession (i.e. comprised of sandstone and ooidal ironstone with lesser conglomerate and siltstone) that typically is about 5 to 15 m thick and exists within...
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View PDF for article title, Stratigraphy of the Bad <span class="search-highlight">Heart</span> <span class="search-highlight">Formation</span>, Clear Hills and Smoky River areas, Alberta
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Journal Article

HOPLOPARIA ALBERTAENSIS , A NEW SPECIES OF CLAWED LOBSTER (NEPHROPIDAE) FROM THE LATE CONIACIAN, SHALLOW-MARINE BAD HEART FORMATION OF NORTHWESTERN ALBERTA, CANADA Available to Purchase

DALE TSHUDY, W. STEVEN DONALDSON, CHRISTOPHER COLLOM, RODNEY M. FELDMANN, CARRIE E. SCHWEITZER
Published: 01 September 2005
Journal of Paleontology (2005) 79 (5): 961–968.
DOI: https://doi.org/10.1666/0022-3360(2005)079[0961:HAANSO]2.0.CO;2
...DALE TSHUDY; W. STEVEN DONALDSON; CHRISTOPHER COLLOM; RODNEY M. FELDMANN; CARRIE E. SCHWEITZER Abstract A new species of clawed lobster, Hoploparia albertaensis , is reported from the late Coniacian, shallow-marine Bad Heart Formation of northwestern Alberta, Canada. Hoploparia is a well-known...
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View PDF for article title, HOPLOPARIA ALBERTAENSIS , A NEW SPECIES OF CLAWED LOBSTER (NEPHROPIDAE) FROM THE LATE CONIACIAN, SHALLOW-MARINE BAD <span class="search-highlight">HEART</span> <span class="search-highlight">FORMATION</span> OF NORTHWESTERN ALBERTA, CANADA
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Journal Article

Basement tectonic control on distribution of the shallow marine Bad Heart Formation: Peace River Arch area, northwest Alberta Available to Purchase

W. Steven Donaldson, A. Guy Plint, Fred J. Longstaffe
Published: 01 December 1998
Bulletin of Canadian Petroleum Geology (1998) 46 (4): 576–598.
DOI: https://doi.org/10.35767/gscpgbull.46.4.576
...W. Steven Donaldson; A. Guy Plint; Fred J. Longstaffe ABSTRACT The late Coniacian Bad Heart Formation in the northwest Alberta Plains is dominated by very fine, variably ooidal sandstone, overlying a dark laminated mudstone. The formation is organised into two principal, sandier-upward sequences...
View PDF for article title, Basement tectonic control on distribution of the shallow marine Bad <span class="search-highlight">Heart</span> <span class="search-highlight">Formation</span>: Peace River Arch area, northwest Alberta
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Journal Article

Sedimentology and subsurface stratigraphy of the Bad Heart Formation of northwestern Alberta Available to Purchase

W.S. Donaldson
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 210–211.
DOI: https://doi.org/10.35767/gscpgbull.39.2.210e
...W.S. Donaldson The Bad Heart Formation of northwestern Alberta is a coarsening-upward package of marine siltstone and sandstone of the Upper Cretaceous Smoky Group. It rests erosionally on the Muskiki and Marshybank formations, the contact being marked by a sideritized pebble bed...
View PDF for article title, Sedimentology and subsurface stratigraphy of the Bad <span class="search-highlight">Heart</span> <span class="search-highlight">Formation</span> of northwestern Alberta
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Journal Article

Revised definitions for the Upper Cretaceous Bad Heart Formation and associated units in the Foothills and Plains of Alberta and British Columbia Available to Purchase

A. Guy Plint, Brett Norris, W. Steven Donaldson
Published: 01 March 1990
Bulletin of Canadian Petroleum Geology (1990) 38 (1): 78–88.
DOI: https://doi.org/10.35767/gscpgbull.38.1.078
...A. Guy Plint; Brett Norris; W. Steven Donaldson RÉSUMÉ Des travaux récents portant sur les formations Coniaciennes-Santoniennes Muskiki, Marshybank et Bad Heart, du groupe Alberta du Crétacé supérieur, ont démontré que les changements de faciès de schiste argileux à microgrès et grès qui marquent...
View PDF for article title, Revised definitions for the Upper Cretaceous Bad <span class="search-highlight">Heart</span> <span class="search-highlight">Formation</span> and associated units in the Foothills and Plains of Alberta and British Columbia
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Journal Article

Morphology and origin of an erosion surface cut into the Bad Heart Formation during major sea-level change, Santonian of west-central Alberta, Canada Available to Purchase

A. Guy Plint, Roger G. Walker
Published: 01 July 1987
Journal of Sedimentary Research (1987) 57 (4): 639–650.
DOI: https://doi.org/10.1306/212F8BC5-2B24-11D7-8648000102C1865D
...A. Guy Plint; Roger G. Walker Abstract Marine sandstones of the early Santonian Bad Heart Formation are up to 50 m thick and are underlain and overlain by marine mudstones of the Muskiki and Puskwaskau Formations, respectively. Our examination of 395 well logs in this stratigraphic interval allowed...
View PDF for article title, Morphology and origin of an erosion surface cut into the Bad <span class="search-highlight">Heart</span> <span class="search-highlight">Formation</span> during major sea-level change, Santonian of west-central Alberta, Canada
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Summary of depositional facies within the Bad Heart Formation (from Donald... Available to Purchase

Published: 01 December 2013
Table 2 Summary of depositional facies within the Bad Heart Formation (from Donaldson, 1997 and Donaldson et al., 1999 ).
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Photograph of the stratigraphy at the Bad Heart Formation type section, which is along the Smoky River just south of the entrance of the Bad Heart River (see Fig. 3 for location). The photograph illustrates (a) the lithostratigrapy which comprises the underlying Kaskapau/Muskiki Formation (Kkk) shales, the Bad Heart Formation (Kbh) sandstone as defined by McLearn, 1919, and the overlying Puskwaskau Formation (Kpw) shales; (b) the erosion surfaces (BES, ES1 and ES) and allomembers (1 and 2) suggested by Donaldson (1997) and Donaldson et al. (1999); (c) the ‘B’ and ‘A’ oolitic markers and proposed Birch Hills member of Collom (2001); and lastly (d) the location of stratigraphic section ASR3C which was geologically mapped by Olson in 2005 (published in Kafle, 2009a). Note that the location of section ASR3B described herein is along the same cliff face, but about 450 m southwest (to the left of section ASR3C).

Photograph of the stratigraphy at the Bad Heart Formation type section, whi... Available to Purchase

Published: 01 December 2013
Figure 5 Photograph of the stratigraphy at the Bad Heart Formation type section, which is along the Smoky River just south of the entrance of the Bad Heart River (see Fig. 3 for location). The photograph illustrates (a) the lithostratigrapy which comprises the underlying Kaskapau/Muskiki
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Comparative stratigraphic interpretations for the Bad Heart Formation type section as proposed by Donaldson et al. (1999), Collom (2001) and the present study. The present study proposes: (a) the Bad Heart Formation continue to be defined on a lithostratigraphic basis (illustrated by red vertical bars), as originally proposed by McLearn (1919), hence at the type section it encompasses only the ‘coarser’ sandstone-siltstone-thin conglomerates which extend from ES1 up to and including those just above ES2, but at section ASR10B1 the lithostratigraphic Bad Heart Formation is much thicker, and extends downwards below ES1 to at least the lowermost sandstone. Further, this study (b) also recognizes three sequence stratigraphic units, SS1 to SS3 (illustrated by blue vertical bars), that extend from the BES in upper lithostratigraphic Kaskapau Formation, encompass the entire Bad Heart Formation, and continue into overlying Puskwaskau Formation shale.

Comparative stratigraphic interpretations for the Bad Heart Formation type ... Available to Purchase

Published: 01 December 2013
Figure 15 Comparative stratigraphic interpretations for the Bad Heart Formation type section as proposed by Donaldson et al. (1999) , Collom (2001) and the present study. The present study proposes: (a) the Bad Heart Formation continue to be defined on a lithostratigraphic basis (illustrated
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Proposed stratigraphic correlation for Bad Heart Formation between the Smoky River (sections ASR3B, ASR10B1 and ASR14C), Peace River (SPRV) and Clear Hills (DDH0203 and Worsley Pit) regions (see Fig. 6 for the legend). Also illustrated is the top and bottom boundaries for the lithostratigraphic Bad Heart Formation as discussed in the text.

Proposed stratigraphic correlation for Bad Heart Formation between the Smok... Available to Purchase

Published: 01 December 2013
Figure 16 Proposed stratigraphic correlation for Bad Heart Formation between the Smoky River (sections ASR3B, ASR10B1 and ASR14C), Peace River (SPRV) and Clear Hills (DDH0203 and Worsley Pit) regions (see Fig. 6 for the legend). Also illustrated is the top and bottom boundaries
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Figure2—Stratigraphic section for Bad Heart Formation at Spirit River Ridge, northwestern Alberta, Canada, indicating locations of specimens described in text (modified from Donaldson et al., 1999). Lobster specimens are indicated by their TMP numbers. *Sample TMP 99.140.100 location projected to this point from sampling locality along Smoky River outcrop approximately 55 km to the southeast

Figure 2 —Stratigraphic section for Bad Heart Formation at Spirit River Ri... Available to Purchase

Published: 01 September 2005
Figure 2 —Stratigraphic section for Bad Heart Formation at Spirit River Ridge, northwestern Alberta, Canada, indicating locations of specimens described in text (modified from Donaldson et al., 1999 ). Lobster specimens are indicated by their TMP numbers. *Sample TMP 99.140.100 location projected
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Scale bar on all figures is equal to 10 μm. Illustrated specimens in the Royal Tyrrell Museum collections have TMP at beginning of specimen number while those in the Geological Survey of Canada collections have a GSC type number. The specimens have been given an unique curation number along with information about the slide number and England Finder location for TMP specimens and an Olympus microscope coordinate for GSC specimens. Figure 1. Callialasporites dampieri (Balme) Dev 1961, Milk River Formation, TMP1989.221.0055, sample 4, slide b, M43/0. Figure 2. Rugubivesiculites reductus Pierce 1961, Milk River Formation, TMP1990.213.0052, sample 1B, slide b,W43/2. Figure 3. Azonia sp. cf. A. pulchella Felix and Burbridge 1973, Cardium Formation, lower Moosehound Member, MDB-82-20, C-104661, P2527-20a, 130.1x10.5, GSC 91382 (Azonia sp., Sweet and McIntyre, 1988, Figure 7–1). Figure 4. Umbosporites callosus Newman 1965, Pakowki Formation, TMP1990.212.0003, sample 3, slide c, J29/4. Figure 5. Azonia pulchella Felix and Burbridge 1973, lower Bad Heart Formation, 6ROCHP016, C-467230, P5002-9d, 123.6x8.6, GSC 133171. Figure 6. Aquilapollenites sp. 1, Milk River Formation, TMP1989.221.0043, sample 4, slide b, T50/0. Figure 7. Fibulapollis punctatus Chlonova 1961 lower Bad Heart Formation, 7ASR11, sample 7SRP008, C-477557, P5053-25e, 121.4x14.8b, GSC 133172. Figure 8. Diptycha sp., upper Bad Heart Formation, 7ASR12, sample 7SRP029, C-477559, P5053-27e, 126.3x14.8 GSC 133173. Figure 9. Jacutiana sp. cf. J. hirsuta Samoilovitch 1965, Bad Heart Formation, 7ASR8E, sample 7SRP024, C-477549, P5053-17e, 123.2x6.9, GSC 133174. Figure 10. Azonia sp. cf. A. jacutense (Samoilovitch) Wiggins 1976, Bad Heart Formation, 7ASR8E, sample 7SRP024, C-477549, P5053- 17e, 123.2x6.9, GSC 133175. Figure 11. Aquilapollenites rombicus Samoilovitch 1965, upper Bad Heart Formation, 7ASR12, sample 7SRP030, C-477560, P5053-28e, 110.6x15.6, GSC 133176. Figure 12. Aquilapollenites sp. cf. A. rombicus Samoilovitch 1965, lower Bad Heart Formation, sample 6ROSRP004, C-467300, P5004-4d, 140.8x6.6, GSC 133177. Figure 13. Tschudypollis thalmannii (Anderson) Nichols 2002, Puskwaskau Formation, 6ROSRP063, C-467334, P5007-8e, 129.8x13.3; GSC 133178. Figure 14. Aquilapollenites senonicus (Mtchedlishvili) Tschudy and Leopold 1971, Milk River Formation, TMP1990.213.0076, sample 2, slide b, K65/1. Figure 15. Kuylisporites scutatus Newman 1965, Foremost Formation, TMP1988.73.0036, sample 76, slide c, D58/0. Figure 16. Accuratipollis lactifluminisBraman 2002, Milk River Formation, TMP1989.221.0041, sample 4, slide c, D58/0. Figure 17. Brevimonosulcites corrugatus Yu and Zhang 1987, Milk River Formation, TMP1989.221.0052, sample 1, slide b, M44/2. Figure 18. Annulispora salsaBraman 2002, Milk River Formation, TMP1989.217.0005, sample 1, slide b, S33/0. Figure 19. Erdtmanipollis circuliferBraman 2002, Milk River Formation, TMP1990.213.0090, sample 1B, slide b, U58/0. Figure 20. Integricorpus scopulensisBraman 2002, Milk River Formation, TMP1989.220.0031, sample 1, slide c, T56/0.

Scale bar on all figures is equal to 10 μm. Illustrated specimens in the Ro... Available to Purchase

Published: 01 June 2012
–1). Figure 4. Umbosporites callosus Newman 1965, Pakowki Formation, TMP1990.212.0003, sample 3, slide c, J29/4. Figure 5. Azonia pulchella Felix and Burbridge 1973, lower Bad Heart Formation, 6ROCHP016, C-467230, P5002-9d, 123.6x8.6, GSC 133171. Figure 6. Aquilapollenites sp. 1, Milk River
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Measured stratigraphic sections in the southern Clear Hills (KC17 to Worsley Pit) and in the eastern Clear Hills at and near Rambling Creek (ARR3 and DDH0203) (refer to Fig. 6 for the Legend). The datum selected for the cross-section is Erosion Surface 1 (ES1). Note that only DDH0203 provides a complete stratigraphy from Kaskapau Formation, across the entire Bad Heart Formation and into overlying Puskwaskau Formation. At the other sections measured in the Clear Hills, typically the uppermost Bad Heart Formation is either poorly exposed due to extensive overburden or has been removed by recent erosion.

Measured stratigraphic sections in the southern Clear Hills (KC17 to Worsle... Available to Purchase

Published: 01 December 2013
provides a complete stratigraphy from Kaskapau Formation, across the entire Bad Heart Formation and into overlying Puskwaskau Formation. At the other sections measured in the Clear Hills, typically the uppermost Bad Heart Formation is either poorly exposed due to extensive overburden or has been removed
Journal Article

An allostratigraphic correlation of the Muskiki and Marshybank formations (Coniacian–Santonian) in the Foothills and subsurface of the Alberta Basin Available to Purchase

A. Guy Plint
Published: 01 September 1990
Bulletin of Canadian Petroleum Geology (1990) 38 (3): 288–306.
DOI: https://doi.org/10.35767/gscpgbull.38.3.288
... topography of several tens of metres. In the eastern part of the area, oolitic sandstones of the Bad Heart Formation (Santonian) rest disconformably on this surface and pass laterally westward into siltstones along a well-defined northwest-southeast-trending line. RÉSUMÉ Les formations Muskiki (Coniacien) et...
View PDF for article title, An allostratigraphic correlation of the Muskiki and Marshybank <span class="search-highlight">formations</span> (Coniacian–Santonian) in the Foothills and subsurface of the Alberta Basin
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Selected wells from sections A–A’ (10a) and B-B’ (10b) to illustrate the details of the sandstone packages within the Bad Heart Formation.

Selected wells from sections A–A’ (10a) and B-B’ (10b) to illustrate the de... Available to Purchase

Published: 01 December 2013
Figure 10 Selected wells from sections A–A’ (10a) and B-B’ (10b) to illustrate the details of the sandstone packages within the Bad Heart Formation.
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Sequence stratigraphic interpretation for Smoky River section ASR10B1 (at right),with the comparative idealized lithofacies succession (at left). The figure shows the lithostratigraphic Bad Heart Formation is a component of the three sequence stratigraphic units, SS1 to SS3, that extend from upper Kaskapau Formation to lower Puskwaskau Formation.

Sequence stratigraphic interpretation for Smoky River section ASR10B1 (at r... Available to Purchase

Published: 01 December 2013
Figure 14 Sequence stratigraphic interpretation for Smoky River section ASR10B1 (at right),with the comparative idealized lithofacies succession (at left). The figure shows the lithostratigraphic Bad Heart Formation is a component of the three sequence stratigraphic units, SS1 to SS3, that extend
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Publicly available oil/gas well logs in the Clear Hills area as of 2006, and the 23 selected wells that were used to construct cross-sections A–A′ and B–B′. Also shown are the Bad Heart Formation stratigraphic sections measured in outcrop or excavated trenches, and two selected industry (Sneddon, 2006) diamond drill cores.

Publicly available oil/gas well logs in the Clear Hills area as of 2006, an... Available to Purchase

Published: 01 December 2013
Figure 4 Publicly available oil/gas well logs in the Clear Hills area as of 2006, and the 23 selected wells that were used to construct cross-sections A–A′ and B–B′. Also shown are the Bad Heart Formation stratigraphic sections measured in outcrop or excavated trenches, and two selected industry
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Measured stratigraphic sections at Smoky River (sections ASR3B to ASR12), and to the northwest (to the left), but south of the Peace River (sections WH4 to BBM). The datum selected for the cross-section is Erosion Surface 2 (ES2). Note that the Bad Heart Formation type section of McLearn (1919) is section ASR3B. Also shown are the approximate position of faults 2 and 3 as inferred by Donaldson et al. (1998).

Measured stratigraphic sections at Smoky River (sections ASR3B to ASR12), a... Available to Purchase

Published: 01 December 2013
Figure 6 Measured stratigraphic sections at Smoky River (sections ASR3B to ASR12), and to the northwest (to the left), but south of the Peace River (sections WH4 to BBM). The datum selected for the cross-section is Erosion Surface 2 (ES2). Note that the Bad Heart Formation type section
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Figure3—Hoploparia albertaensis n. sp. from the late Coniacian Bad Heart Formation of northwestern Alberta, Canada. 1, 2 (TMP 2001.9.2; paratype), Left lateral and dorsal views; 3–5 (TMP 2001.9.3; holotype), right lateral and dorsal views of cephalothorax and abdomen; 6 (TMP 2001.9.5; paratype), left lateral view of cephalothorax; 7 (TMP 94.140.100; paratype), right oblique view of cephalothorax and unequal claws. Scale bars equal 1.0 cm

Figure 3 — Hoploparia albertaensis n. sp. from the late Coniacian Bad Hea... Available to Purchase

Published: 01 September 2005
Figure 3 — Hoploparia albertaensis n. sp. from the late Coniacian Bad Heart Formation of northwestern Alberta, Canada. 1, 2 (TMP 2001.9.2; paratype), Left lateral and dorsal views; 3 – 5 (TMP 2001.9.3; holotype), right lateral and dorsal views of cephalothorax and abdomen; 6 (TMP 2001.9.5
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Figure 2.

Field photographs. (a) The Black Heart dyke and the Ardon Formation, lookin... Available to Purchase

Published: 29 October 2013
Figure 2. Field photographs. (a) The Black Heart dyke and the Ardon Formation, looking north. O.M.B is 189 cm tall for scale. (b) Appearance of the geode-bearing grey veins adjacent to the dyke. (c) In situ appearance of the round geodes. (d