Publications in Karnes
Title | Publication Year Sort ascending | Abstract | Author | Series | Publisher | |
---|---|---|---|---|---|---|
![]() |
Depositional and ground-water flow systems of the Carrizo - Upper Wilcox, south Texas | 1988 | In the Rio Grande Embayment of South Texas, the Carrizo Formation (lower Eocene) consists of two sand-rich fluvial depositional systems that grade basinward into several deltaic complexes within the upper part of the Wilcox Group. |
Hamlin, H.S. | Report of Investigations | Bureau of Economic Geology |
![]() |
The Guadalupe - Lavaca - San Antonio - Nueces River basins regional study: Seguin West - Austin West sheets | 1985 | Wermund, E.G., Gustavson, T.C., Morton, R.A., Woodruff, C.M., Jr., Macpherson, G.L., McKinney, L., Nilsson, J., Waddell, C.T. | River Basins Regional Studies | Bureau of Economic Geology | |
![]() |
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 | 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 | 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 | 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 In 1976, approximately 6,000 acre-ft of ground water were withdrawn from the Oakville for municipal use.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 |
![]() |
Upper Tertiary and Quaternary depositional systems, central coastal plain, Texas -- regional geology of the coastal aquifer and potential liquid-waste repositories | 1981 | Upper Miocene, Pliocene, and Pleistocene deposits in the subsurface of the central Coastal Plain of Texas were subdivided into six operational units comprising the surface-defined Fleming, Goliad, Willis, Lissie, and Beaumont Formations. |
Solis-Iriarte, R.F. | Report of Investigations | Bureau of Economic Geology |
![]() |
Depositional and diagenetic history of the Sligo and Hosston Formations(Lower Cretaceous) in south Texas | 1981 | The Sligo and Hosston Formations of Aptian age occur over thousands of square miles in the subsurface of South Texas. |
Bebout, D.G., Budd, D.A., Schatzinger, R.A. | Report of Investigations | Bureau of Economic Geology |
![]() |
Smackover and lower Buckner Formations, south Texas: depositional systems on a Jurassic carbonate ramp | 1981 | The Smackover and lower part of the Buckner Formations (Oxfordian) comprise a thick regressive sedimentary sequence deposited on a Jurassic carbonate ramp. Four major depositional systems are recognized: (1) basinal, (2) low-energy open shelf, (3) high-energy shoal, and (4) sabkha. |
Budd, D.A., Loucks, R.G. | Report of Investigations | Bureau of Economic Geology |
![]() |
Structural cross sections, Tertiary formations, Texas Gulf Coast | 1981 | The publication comprises 24 structural dip cross sections, spaced 15 to 20 mi apart along the Texas coast, and 4 structural strike cross sections. Dip sections extend from near the Wilcox outcrop to the coastline. |
Dodge, M.M., Posey, J.S. | Cross Sections | Bureau of Economic Geology |