Earth:Favel Formation
| Favel Formation Stratigraphic range: Late Cenomanian-mid Turonian ~95–90 Ma | |
|---|---|
| Type | Formation |
| Sub-units | Assiniboine Member Keld Member |
| Underlies | Morden Formation |
| Overlies | Belle Fourche Formation |
| Thickness | Up to about 46 m (151 ft)[1] |
| Lithology | |
| Primary | Calcareous shale |
| Other | Argillaceous limestone, calcarenite, bentonite |
| Location | |
| Coordinates | [ ⚑ ] : 52°08′36″N 100°58′38″W / 52.14333°N 100.97722°W |
| Region |  Saskatchewan Manitoba |
| Country |  Canada |
| Type section | |
| Named for | Favel River, Manitoba |
| Named by | R.T.D. Wickenden[2] |
| Year defined | 1945 |
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The Favel Formation is a stratigraphic unit of Late Cretaceous (late Cenomanian to middle Turonian) age. It is present in southern Manitoba and southeastern Saskatchewan, and consists primarily of calcareous shale. It was named for the Favel River near Minitonas, Manitoba, by R.T.D. Wickenden in 1945.[1][2]
The Favel Formation is richly fossiliferous and had yielded remains of a wide variety of marine animals, including the marine crocodile Terminonaris.[3][4] It is also rich in organic carbon and is therefore an oil shale.[5]
Lithology and thickness
The Favel Formation is subdivided into the upper Assiniboine Member and the lower Keld Member. Both consist primarily of olive-black, chalk-speckled, calcareous and carbonaceous shale, with lesser amounts of shaly and argillaceous limestone, minor beds of calcarenite, and numerous thin beds of bentonite. The Assiniboine Member is topped by a bed of shaly argillaceous limestone called the Marco Calcarenite. The Keld is more calcareous than the Assiniboine, and is topped by a bed of shaly argillaceous limestone called the Laurier Limestone.[1][4] The Marco and Laurier marker beds are notable for their strong "kicks" in well logs, and so are useful in identifying subsurface formations.
The Favel Formation reaches a maximum thickness of 46 m (151 ft) in southern Manitoba.[1]
Deposition and paleontology
The Favel Formation was deposited along the eastern edge of the Western Interior Seaway. The water was anoxic at depth, which was conducive to the preservation of fossils and organic matter.[6]
Numerous fossils have been recovered from the Favel Formation. There are remains of coccoliths and planktonic foraminifera, aggregates of which make up the formation's distinctive the "chalk specks". Invertebrates include the bivalves Inoceramus, Mytilloides, and Ostrea, and ammonites such as Collignoniceras. There are bony fishes, including articulated specimens of Xiphactinus audax, as well as Apsopelix, Pachyrhizodus, and others. Cartilagenous fishes include sharks such as Odontaspis, Squalicorax, and Ptychodus, as well as rays.[7] The largely complete skeleton of the marine crocodyliform Terminonaris robusta (first described as Teleorhinus robustus), was recovered from the Keld Member about 1 m (3 ft) below the Laurier Limestone bed,[7] and has been nicknamed "Big Bert".
Distribution and relationship to other units
The Favel Formation is present in the subsurface beneath the plains of southern Manitoba and southeastern Saskatchewan, and can be seen in outcrop in river valleys along the Manitoba Escarpment and the Pasquia Hills. Its contact with the noncalcareous shales of the Ashville Formation is conformable to unconformable, depending on the location, and the formation is unconformably overlain by the noncalcareous shales of the Morden Formation. To the west it is equivalent to the Second White Speckled Shale of the Colorado Group, and the Vimy Member of the Blackstone Formation.[1][8][9]
In structure and fossil age, the Keld member correlates with the Greenhorn units widely identified in the Great Plains and within the Mancos Shale. The fossils (C. woollgari and I. labiatis) and well log indications of the top of the Greenhorn (Fencepost limestone) particularly correlate with the Laurier Limestone bed.[10]
Economic resources
The Favel Formation is an oil shale. It is rich in kerogen, with a total organic carbon content that ranges up to 10%. Fresh samples typically have a petroliferous odor. Because they were deposited under marine conditions, the Favel shales are classified as marinites, in contrast to the lamosite oil shales of the Green River Formation, which were deposited in a lacustrine environment. The formation may also have some potential for biogenic natural gas.[5]
See also
- List of fossiliferous stratigraphic units in Manitoba
References
- ↑ 1.0 1.1 1.2 1.3 1.4 Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba, p. 74, 440, & 631. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. ISBN:0-920230-23-7.
- ↑ 2.0 2.1 Wickenden, R.T.D. 1945. Mesozoic stratigraphy of the eastern plains, Manitoba and Saskatchewan. Geological Survey of Canada, Memoir 239.
- ↑ Collom, C.J. 2000. High-resolution stratigraphy, regional correlation, and report of molluscan faunas: Colorado Group (Cenomanian – Coniacian) interval, Late Cretaceous, east-central Saskatchewan. In: Summary of Investigations 2000, Vol. 1, Saskatchewan Geological Survey, Sask. Energy Mines, Miscellaneous Report 2000-4.1, p. 82-97
- ↑ 4.0 4.1 Christopher, J., Yurkowski, M., Nicolas, M. and Bamburak, J. 2006. The Cenomanian–Santonian Colorado formations of eastern southern Saskatchewan and southwestern Manitoba. In: C.F. Gilboy and S.G. Whittaker (eds.), Saskatchewan and Northern Plains Oil and Gas Symposium 2006, Saskatchewan Geological Society, Special Publication 19, p. 299-318.
- ↑ 5.0 5.1 Macauley, G. 1984. Cretaceous oil shale potential in Saskatchewan. In: J.A. Lorsong and M.A. Wilson, eds., Oil and Gas in Saskatchewan, proceedings of a conference held in Regina, Saskatchewan, 11-12 October 1984; p. 255-269.
- ↑ Schröder-Adams, C.J., Cumbaa, S.L., Bloch, J., Leckie, D.A., Craig, J., Seif el-Dein, S.A., Simons, D.-J.H.A.E. and Kenig, F. 2001. Late Cretaceous (Cenomanian to Campanian) paleoenvironmental history of the eastern Canadian margin of the Western Interior Seaway: bonebeds and anoxic events. Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 170, p. 261-289.
- ↑ 7.0 7.1 Cumbaa, S.L. and Tokaryk, T.S. 1999. Recent discoveries of Cretaceous marine vertebrates on the eastern margins of the Western Interior Seaway. In: Summary of Investigations 1999, Vol. 1, Saskatchewan Geological Survey, Sask. Energy Mines, Miscellaneous Report 99-4.1, p. 57-63.
- ↑ Williston Basin TGI, 2009. "Stratigraphic Correlation Chart, TGI II: Williston Basin architecture and hydrocarbon potential in eastern Saskatchewan and western Manitoba". https://www.gov.mb.ca/iem/geo/willistontgi/downloads/tgi_strat_column.pdf. Retrieved 20 June 2021.
- ↑ Saskatchewan Industry and Resources, 2004. "Saskatchewan Stratigraphic Correlation Chart". http://www.ir.gov.sk.ca/files/co2monitoring/PDFs/strat%20char.pdf. Retrieved 20 June 2021.
- ↑ Donald E. Hattin (1975). Stratigraphy and Depositional Environment of Greenhorn Limestone (Upper Cretaceous) of Kansas, Kansas Geological Survey, Bulletin 209. University of Kansas Publications, State Geological Survey of Kansas. p. Depositional Environment and Paleoecology. http://www.kgs.ku.edu/Publications/Bulletins/209/07_paleo.html. "North of the Canadian border, the Greenhorn is not recognized as a formal unit, but its position is recognized in the Favel Formation (second speckled shale unit of petroleum geologists) in Manitoba and Saskatchewan (Wickenden, 1945, p. 33)."
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