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Publications in Refugio

Title Publication Year Sort ascending Abstract Author Series Publisher
Shoreline and vegetation-line movement, Texas Gulf coast, 1974 to 1982 Shoreline and vegetation-line movement, Texas Gulf coast, 1974 to 1982 1989

The purposes of this study were (1) to quantify recent (1974 to 1982) movement of Texas shorelines and vegetation lines by analysis of aerial photographs; (2) to place this movement in historical (pre-1974) context; and (3) to examine the influence of environmental variables such as storms, sea l

Paine, J.G., Morton, R.A. Geological Circular Bureau of Economic Geology
Hydrocarbon production and exploration potential of the distal Frio Formation, Texas Gulf coast and offshore Hydrocarbon production and exploration potential of the distal Frio Formation, Texas Gulf coast and offshore 1989

Along the Texas Gulf shoreline and offshore, the distal margin of the Frio Formation is a deep hydrocarbon province that is underexplored relative to the onshore Frio.

Hamlin, H.S. Geological Circular Bureau of Economic Geology
Submerged lands of Texas, Port Lavaca area:  sediments, geochemistry, benthic macroinvertebrates, and associated wetlands Submerged lands of Texas, Port Lavaca area: sediments, geochemistry, benthic macroinvertebrates, and associated wetlands 1989

The State-owned submerged lands of Texas encompass almost 6,000 mi2 (15,540 km2). They lie below waters of the bay-estuary-lagoon system and the Gulf of Mexico and extend 10.3 mi (16.6 km) seaward from the Gulf shoreline (fig. 1).

White, W.A., Calnan, T.R., Morton, R.A., Kimble, R.S., Littleton, T.G., McGowen, J.H., Nance, H.S. Submerged Lands of Texas Bureau of Economic Geology
Historical shoreline changes in San Antonio, Espiritu Santo, and Mesquite Bays, Texas Gulf coast Historical shoreline changes in San Antonio, Espiritu Santo, and Mesquite Bays, Texas Gulf coast 1987

Changes in the position and stability of shorelines in the San Antonio Bay system (San Antonio, Espiritu Santo, and Mesquite Bays), Texas Gulf Coast, were documented using historical monitoring techniques.

White, W.A., Morton, R.A. Geological Circular Bureau of Economic Geology
Submerged lands of Texas, Corpus Christi area:  sediments, geochemistry, benthic macroinvertebrates, and associated wetlands Submerged lands of Texas, Corpus Christi area: sediments, geochemistry, benthic macroinvertebrates, and associated wetlands 1983

The State-owned submerged lands of Texas encompass almost 6,000 mi2 (15,540 km2). They lie below waters of the bay-estuary-lagoon system and the Gulf of Mexico and extend 10.3 mi (16.6 km) seaward from the Gulf shoreline (fig. 1).

White, W.A., Calnan, T.R., Morton, R.A., Kimble, R.S., Littleton, T.G., McGowen, J.H., Nance, H.S., Schmedes, K.E. Submerged Lands of Texas 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
Upper Tertiary and Quaternary depositional systems, central coastal plain, Texas -- regional geology of the coastal aquifer and potential liquid-waste repositories 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
Structural cross sections, Tertiary formations, Texas Gulf Coast 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