Debolt Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Rundle Group |
Sub-units | Upper Debolt Lower Debolt |
Underlies | Golata Formation |
Overlies | Shunda Formation |
Thickness | up to 366 metres (1,200 ft)[1] |
Lithology | |
Primary | Limestone, dolomite |
Other | Shale, anhydrite |
Location | |
Coordinates | 55°18′21″N 117°53′46″W / 55.3057°N 117.8961°W |
Region | Alberta, British Columbia |
Country | Canada |
Type section | |
Named for | Debolt, Alberta |
Named by | G. Macauley, 1958 |
The Debolt Formation is a stratigraphical unit of Meramecian age in the Western Canadian Sedimentary Basin.
It takes the name from the hamlet of Debolt, Alberta, and was first described in the Amerada Crown GF23-11 well near Debolt by G. Macauley in 1958.[2]