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Rundle Group : ウィキペディア英語版
Rundle Group

The Rundle Group is a stratigraphical unit of Mississippian age in the Western Canadian Sedimentary Basin.
It takes the name from Mount Rundle (itself taking the name from Robert Terrill Rundle), and was first described in outcrops at the northern side of the mountain in Banff National Park by R.J.W. Douglas in 1953.〔Douglas, R.J.W., 1953b. Carboniferous stratigraphy in the southern Foothills of Alberta; Alberta Soc. Petrol. Geol., 3rd Ann. Field Conf. Guidebook, p. 66-88.〕
==Lithology==
The Rundle Group consists of massive limestone interbedded with dark argillaceous limestone. Chert nodules are observed in the shaley beds, and crinoids and brachiopods are observed in the clean massive beds.〔 Dolimitization is observed in the Elkton Member of the Turner Valley Formation.

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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