Английская Википедия:Garber Sandstone

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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.[1]

The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.[2]

See also

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References

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Шаблон:Oklahoma-geologic-formation-stub Шаблон:Permian-stub

  1. The Garber-Wellington Aquifer, Association of Central Oklahoma Governments
  2. 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