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Utica Shale : ウィキペディア英語版
Utica Shale

The Utica Shale is a stratigraphical unit of Middle Ordovician age in the Appalachian Basin. It
underlies much of the northeastern United States and adjacent parts of Canada.
It takes the name from the city of Utica, New York, as it was first described as an outcrop along the Starch Factory Creek east of the city by Ebenezer Emmons in 1842.〔Emmons, Ebenezer, 1842, Geology of New York; Part II, Survey of the second geological district: New York State Museum, 437p.〕
==Lithology==
The Utica Shale is composed of calcareous, organic, and rich shale.〔

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「Utica Shale」の詳細全文を読む



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