Grosmont Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Woodbend Group |
Sub-units | Hondo Member |
Underlies | Nisku Formation, McMurray Formation |
Overlies | Ireton Formation, Duvernay Formation |
Thickness | up to 230 metres (750 ft)[1] |
Lithology | |
Primary | Limestone, dolomite |
Other | siltstone, shale |
Location | |
Coordinates | 58°22′N 114°55′W / 58.367°N 114.917°W |
Region | WCSB |
Country | Canada |
Extent | 100,000 square kilometres (38,610 sq mi) |
Type section | |
Named for | Grosmont, Alberta |
Named by | H.R. Belyea, 1952 |
The Grosmont Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.
It takes the name from the hamlet of Grosmont, Alberta, and was first described in well Imperial Grosmont No. 1, in 13-17-67-23W4M, central Alberta by H.R. Belyea in 1952.[2]
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