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Publications by Smith, G.E.

Title Publication Year Abstract Author Series Publisher
Depositional framework, hydrostratigraphy, and uranium mineralization of the Oakville Sandstone (Miocene), Texas coastal plain Depositional framework, hydrostratigraphy, and uranium mineralization of the Oakville Sandstone (Miocene), Texas coastal plain 1982

The Oakville Sandstone (Miocene) of the Texas Coastal Plain comprises a major sand-rich fluvial system composed of deposits of several major and minor rivers that originated within Texas and surrounding states.

Galloway, W.E., Henry, C.D., Smith, G.E. Report of Investigations Bureau of Economic Geology
Geochemistry of ground water in the Miocene Oakville Sandstone -- a major aquifer and uranium host of the Texas coastal plain Geochemistry of ground water in the Miocene Oakville Sandstone -- a major aquifer and uranium host of the Texas coastal plain 1982

The Oakville Sandstone is a major aquifer and a major host of uranium deposits in the Texas Coastal Plain.

Henry, C.D., Galloway, W.E., Smith, G.E., Ho, C.L., Morton, J.P., Gluck, J.K. Report of Investigations Bureau of Economic Geology
Regional hydrodynamics and hydrochemistry of the uranium-bearing Oakville aquifer (Miocene) of south Texas Regional hydrodynamics and hydrochemistry of the uranium-bearing Oakville aquifer (Miocene) of south Texas 1982

The Oakville Formation consists of sediments deposited by several major fluvial systems that traversed the Texas Coastal Plain during the Miocene Epoch.

Smith, G.E., Galloway, W.E., Henry, C.D., Gluck, J.K., McIntyre, J.F., Pisasale, E.T., Spradlin, S.D. Report of Investigations Bureau of Economic Geology
Considerations in the extraction of uranium from a fresh-water aquifer -- Miocene Oakville Sandstone, south Texas Considerations in the extraction of uranium from a fresh-water aquifer -- Miocene Oakville Sandstone, south Texas 1982

The Miocene Oakville Sandstone is a major aquifer and uranium host beneath the Texas Coastal Plain. In 1976, approximately 6,000 acre-ft of ground water were withdrawn from the Oakville for municipal use.

Henry, C.D., Galloway, W.E., Smith, G.E., Childs, C.S., Devine, P.E., Dutton, A.R., Gluck, J.K., McIntyre, J.F. Report of Investigations Bureau of Economic Geology
Depositional systems, San Angelo Formation (Permian), north Texas -- facies control of red-bed copper mineralization Depositional systems, San Angelo Formation (Permian), north Texas -- facies control of red-bed copper mineralization 1974

The San Angelo Formation is a mid-Permian sandstone and mudstone sequence about 100 feet thick that crops out in North Texas and dips westward into the Midland Basin; it is composed of two superposed members: the basal Duncan Sandstone Member and the overlying Flowerpot Mudstone Member.

Smith, G.E. Report of Investigations Bureau of Economic Geology