Blairmore Group

Blairmore Group
Stratigraphic range: Early Cretaceous
Blairmore Group; Stratigraphic range: Early Cretaceous
Type	Group
Sub-units	Cadomin Formation, Gladstone Formation, Beaver Mines Formation, Ma Butte Formation
Underlies	Crowsnest Formation, Alberta Group
Overlies	Kootenay Group
Thickness	up to 2,000 m (6,560 ft)[1]
Lithology
Primary	Sandstone, siltstone, mudstone
Other	Conglomerate, limestone
Location
Region	Alberta British Columbia
Country	Canada
Type section
Named for	Blairmore, Alberta
Named by	W.W. Leach, 1914[2]

The Blairmore Group, originally named the Blairmore Formation, is a geologic unit of Early Cretaceous age in the Western Canada Sedimentary Basin that is present in southwestern Alberta and southeastern British Columbia.[1][3] It is subdivided into a series of formations, most of which contain plant fossils. In some areas it contains significant reservoirs of natural gas.

Lithology

The Blairmore group includes the conglomerate and quartzose sandstones of the Cadomin Formation at the base, and grades to sandstone, siltstone, mudstone, and limestone in the overlying formations. The Beaver Mines and Ma Butte Formations in the upper part of the group also include minor beds of bentonite and tuff.[1]

Stratigraphy

The Blairmore Group is subdivided into the following formations from top to base:

Formation	Age	Lithology	Max Thickness	Reference
Ma Butte Formation	Early Cretaceous	mudstone, siltstone, very fine-grained sandstone, bentonite and tuff	120 m (390 ft)	[1]
Beaver Mines Formation	Early Cretaceous	greenish grey sandstone and mudstone; minor conglomerate, bentonite and tuff	455 m (1,490 ft)	[1]
Gladstone Formation	Early Cretaceous	argillaceous limestone and calcareous shale	180 m (590 ft)	[1]
Cadomin Formation	Early Cretaceous	conglomerate, sandstone	170 m (560 ft)	[1]

Some early workers included the Crowsnest Formation, which overlies the Ma Butte Formation, at the top of the Blairmore Group, but that practice has been abandoned.[1]

Distribution and Thickness

The name Blairmore Group is applicable in the foothills and mountains of southwestern Alberta and southeastern British Columbia, from the Canada–United States border northward to the Clearwater River. The equivalent strata north of the Clearwater River, which were originally assigned to the Blairmore Group, differ in that they contain major coal deposits and they have therefore been reassigned to the Luscar Group.[4]

The Blairmore Group has a maximum thickness of about 2,000 m (6,560 ft) and thins from west to east.[1]

Relationship to other units

The Blairmore Group unconformably overlies the Kootenay Group and is gradationally overlain by the Crowsnest Formation or, where the Crowsnest Formation is absent, is disconformably overlain by the Alberta Group. It is equivalent to the Luscar Group north of the Clearwater River[4] and to the Mannville Group in the plains to the east.[1]

Environment of deposition and paleontology

The Blairmore Group is an eastward-thinning wedge of clastic sediments derived from the erosion of newly uplifted mountains to the west. The sediments were transported eastward by river systems and deposited in a variety of braided stream, river channel, floodplain, and coastal plain environments along the western edge of the Western Interior Seaway. Its formations include a variety of plant fossils, trace fossils, bivalves, and mircofossils.

gollark: Okay, even if you don't need ATM-stolen levels of security, it still needs to be ridiculously secure.

gollark: Also, can you not, say, invisibly read from an RFID card someone had and take all their money?

gollark: That answer to 4.

gollark: Sorry. What?!

gollark: I can see a few problems:1. how are you planning to make secure bank cards?2. how will people trust the system?3. how is it actually more convenient than holding [CURRENCY] in your inventory?4. you will need it to be really secure - so secure that even if an ATM is stolen it won't be possible to meddle with the backend.

References

Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. ISBN 0-920230-23-7.
Leach, W.E. 1914. Blairmore map-area, Alberta. Geological Survey of Canada, Summary Report 1912, Map 107A.
Canadian Society of Petroleum Geologists and Alberta Geological Survey (1994). "The Geological Atlas of the Western Canada Sedimentary Basin, Chapter 19: Cretaceous Mannville Group of the Western Canada Sedimentary Basin". Compiled by Mossop, G.D. and Shetsen, I. Archived from the original on 2016-07-01. Retrieved 2016-06-20.
Langenberg, W.C. and McMechan, M.E. 1985. Lower Cretaceous Luscar Group (revised) of the northern and north-central foothills of Alberta. Bulletin of Canadian Petroleum Geology, v. 33, p. 1-11.

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.

[Glass-1] Glass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. ISBN 0-920230-23-7.

[Leach-2] Leach, W.E. 1914. Blairmore map-area, Alberta. Geological Survey of Canada, Summary Report 1912, Map 107A.

[Mossop19-3] Canadian Society of Petroleum Geologists and Alberta Geological Survey (1994). "The Geological Atlas of the Western Canada Sedimentary Basin, Chapter 19: Cretaceous Mannville Group of the Western Canada Sedimentary Basin". Compiled by Mossop, G.D. and Shetsen, I. Archived from the original on 2016-07-01. Retrieved 2016-06-20.

[Langenberg-4] Langenberg, W.C. and McMechan, M.E. 1985. Lower Cretaceous Luscar Group (revised) of the northern and north-central foothills of Alberta. Bulletin of Canadian Petroleum Geology, v. 33, p. 1-11.