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Garber Sandstone : ウィキペディア英語版 | Garber Sandstone
The Garber Sandstone is a geologic formation from the Permian Period in Oklahoma. It serves as an important aquifer, the Garber-Wellington Aquifer, in Logan, Oklahoma, and Cleveland counties of central Oklahoma.〔(The Garber-Wellington Aquifer, Association of Central Oklahoma Governments ) 〕 The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.〔''Review of the General Geology and Solid-Phase Geochemical Studies in the Vicinity of the Central Oklahoma Aquifer,'' US Geological Survey Circular 1019, 1986, p. 6 〕 ==See also==
* List of fossiliferous stratigraphic units in Oklahoma
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「Garber Sandstone」の詳細全文を読む
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