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.[2]
The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the outcrop area.[3]
See also
References
- ^ a b Garber Sandstone, USGS: Mineral Resources > Online Spatial Data
- ^ The Garber-Wellington Aquifer, Association of Central Oklahoma Governments
- ^ 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