The Luscar Group is a geologic unit of Early Cretaceous age in the Western Canada Sedimentary Basin that is present in the foothills of southwestern Alberta.[1][2] It is subdivided into a series of formations, some of which contain economically significant coal deposits that have been mined near Cadomin and Luscar.[3] Coal mining in those areas began in the early 1900s[4] and continues near Luscar as of 2016.
| Luscar Group | |
|---|---|
| Stratigraphic range: | |
| Type | Group |
| Sub-units | Cadomin Formation, Gladstone Formation, Moosebar Formation, Gates Formation |
| Underlies | Blackstone Formation, Shaftesbury Formation |
| Overlies | Nikanassin Formation, Minnes Group |
| Thickness | about 145 m (480 ft) |
| Lithology | |
| Primary | Sandstone, siltstone, mudstone |
| Other | Coal, conglomerate |
| Location | |
| Coordinates | 53°01′57″N 117°19′35″W / 53.03246°N 117.32652°W |
| Region |  Alberta |
| Country |  Canada |
| Type section | |
| Named for | Luscar, Alberta |
| Named by | C.W. Langenberg and M.E. McMechan, 1985[1] |
  Luscar Group (Canada) | |
Lithology
editThe Luscar Group includes the conglomerate and quartzose sandstones of the Cadomin Formation at the base, and the overlying formations consist of variable amounts of sandstone, siltstone and mudstone. There are major coal seams in the Gates Formation, and minor coal, argillaceous limestone and calcareous shale in the Gladstone Formation. The Moosebar Formation consists primarily of mudstone and shale.[1][5]
Stratigraphy
editThe strata encompassed by the Luscar Group were originally included in the Blairmore Group. However, the Blairmore Group strata in the mountains and foothills of southwestern Alberta are of primarily nonmarine origin and are not coal-bearing, while those in the central and northern foothills include thick coal seams and a marine shale unit. Those strata were therefore reassigned to the Luscar Group. [1][5]
The type section for the Luscar Group consists of outcrops along the railroad tracks near the town of Cadomin.[1]
Luscar Group is subdivided into the following formations from top to base:
| Formation | Age | Lithology | Max Thickness |
Reference |
|---|---|---|---|---|
| Gates Formation | early Albian | sandstone, siltstone, mudstone, coal; minor conglomerate | 345 m (1,130 ft) | [5][6] |
| Moosebar Formation | early Albian | grey mudstone; minor siltstone | 60 m (200 ft) | [5][6] |
| Gladstone Formation | Aptian to Albian | fine-grained sandstone, siltstone mudstone; minor limestone and coal | 115 m (380 ft) | [5][6] |
| Cadomin Formation | Aptian | conglomerate, sandstone | 45 m (150 ft) | [5][6] |
Distribution and thickness
editThe name Luscar Group is applicable in the northern and north-central foothills of southwestern Alberta, from the Clearwater River north to the Kakwa River near the Alberta-British Columbia boundary. Its thickness is difficult to determine accurately due to folding and faulting that characterize the Alberta foothills, but is estimated to be about 145 m (480 ft) in the type area.[1]
Relationship to other units
editThe Luscar Group is correlative with the Blairmore Group of the southwestern Alberta foothills; with the Bullhead Group and the lower part of the Fort St. John Group of northeastern British Columbia; and with the Mannville Group of the Alberta plains.[1][2] It disconformably overlies either the Nikanassin Formation or the Minnes Group, and is disconformably overlain by either the Shaftesbury Formation or Blackstone Formation, depending on the location.[1]
Environment of deposition and paleontology
editThe Luscar 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, swamp, coastal plain, marginal marine and shallow marine environments along the western edge of the Western Interior Seaway.[2][5] Its formations include a variety of plant fossils, trace fossils, bivalves, and foraminifera.[5]
References
edit- ^ a b c d e f g h Langenberg, C.W. and McMechan, M.E. 1985. Lower Cretaceous Luscar Group (revised) of the northern and north-central foothills of Alberta. Bulletin of Canadian Petroleum Geology, vol. 33, p. 1-11.
- ^ a b c Mossop, G.D. and Shetsen, I. (compilers), 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". Retrieved 2016-06-20.
{{cite web}}: CS1 maint: multiple names: authors list (link) - ^ Mossop, G.D. and Shetsen, I. (compilers), Canadian Society of Petroleum Geologists (1994). "The Geological Atlas of the Western Canada Sedimentary Basin, Chapter 33: Coal Resources of the Western Canada Sedimentary Basin". Retrieved 2016-06-20.
{{cite web}}: CS1 maint: multiple names: authors list (link) - ^ Ross, Toni (1999). Oh! The Coal Branch. Calgary, Alberta: D.W. Friesen and Sons Ltd., 240 p. ISBN 0-919212-51-4.
- ^ a b c d e f g h Langenberg, C.W. 1984. Structural and sedimentological framework of the Lower Cretaceous coal-bearing rocks of the Grande Cache area, Alberta. In: The Mesozoic of Middle North America, Canadian Society of Petroleum Geologists Memoir 9, p. 533-540.
- ^ a b c d 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.