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Rainbow Member : ウィキペディア英語版
Keg River Formation

The Keg River Formation is a stratigraphic unit of Givetian age in the Western Canada Sedimentary Basin.
It takes the name from the Keg River, a tributary of the Peace River, and was first described in the California Standard Steen River 2-22-117-5W6M well (situated north of Zama Lake) by J. Law in 1955.
==Lithology==
The Keg River Formation is composed of dark dolostone with intercrystalline or vuggy porosity and wackestone limestone.


The Rainbow Member and upper Keg River Member are reef formations deposited in the Rainbow, Zama and Bitscho sub-basins.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Keg River Formation」の詳細全文を読む



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