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Crowfoot Formation : ウィキペディア英語版
Crowfoot Formation

The Crowfoot Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin.
It takes the name from Crowfoot Creek, a tributary of the Bow River and was first described in the ''Royalite Crowfoot No. 2'' well, located near the creek by H.R. Belyea and D.J. McLaren in 1957. 〔Belyea, H.R. and McLaren, D.J., 1957. Upper Devonian nomenclature in southern Alberta. Journal of the Alberta Society of Petroleum Geologists, v. S. p.166-182.〕
==Lithology==
The Crowfoot Formation consists of anhydrite, silty dolomite, with minor shale.



抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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