Breadcrumb
Bureau of Economic Geology Publications
| Title | Publication Year Sort ascending | Abstract | Author | Publisher | |
|---|---|---|---|---|---|
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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. | Bureau of Economic Geology |
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Hydrogeology of Barbers Hill salt dome, Texas coastal plain | 1988 | Barbers Hill salt dome, located in the Texas Coastal Plain near Houston, has a long history of resource exploitation, including oil and brine production, storage of hydrocarbons in solution-mined caverns within the salt stock, and disposal of brine into the cap rock. |
Hamlin, H.S., Smith, D.A., Akhter, M.S. | Bureau of Economic Geology |
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Hydrogeology and hydrochemistry of the Ogallala aquifer, southern High Plains, Texas panhandle and eastern New Mexico | 1988 | The Ogallala aquifer, which underlies the Southern High Plains, consists of the saturated sediments of the Neogene Ogallala Formation. The aquifer is the main source of water for the High Plains of Texas and New Mexico and is being severely depleted by extensive pumpage for irrigation. |
Nativ, Ronit | Bureau of Economic Geology |
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Effects of facies and diagenesis on reservoir heterogeneity: Emma San Andres field, West Texas | 1988 | Pervasively dolomitized, anhydritic carbonates of the upper San Andres Formation in the Emma field of West Texas constitute an upward-shallowing sequence of lithofacies representing four major depositional environments. |
Ruppel, S.C., Cander, H.S. | Bureau of Economic Geology |
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Regional structural cross sections, mid-Permian to Quaternary strata, Texas panhandle and eastern New Mexico: distribution of evaporites and areas of evaporite dissolution and collapse | 1988 | The Palo Duro Basin of the Texas Panhandle and eastern New Mexico contains bedded Permian salts of sufficient thickness and depth for the basin to be considered as a potential site for long-term storage and isolation of high-level nuclear waste. |
McGookey, D.A., Gustavson, T.C., Hoadley, A.D. | Bureau of Economic Geology |
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An Assessment of the Natural Gas Resource Base of the United States | 1988 | Natural gas in the United States consists of proved reserves in known reservoirs, of inferred reserves and undeveloped resources within these reservoirs, and of undiscovered resources. |
Finley, R.J., Fisher, W.L., Seni, S.J., Ruppel, S.C., White, W.G., Ayers Jr., W.B., Dutton, S.P., Jackson, M.L.W. | Bureau of Economic Geology |
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Geomorphic processes and rates of retreat affecting the Caprock Escarpment, Texas panhandle | 1988 | The interaction of geomorphic and ground-water processes has produced the Caprock Escarpmentthat bounds the eastern margin of the Southern High Plains in the Texas Panhandle. |
Gustavson, T.C., Simpkins, W.W. | Bureau of Economic Geology |
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The Mineral Industry of Texas in 1986 | 1988 | Ohl, J.P., McBride, M.W. | Bureau of Economic Geology | |
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A saponite and chlorite-rich clay assemblage in Permian evaporite and red-bed strata, Palo Duro basin, Texas panhandle | 1987 | Permian strata in the Palo Duro Basin consist of multicyclic sequences of carbonate, nodular and laminated anhydrite, bedded halite, chaotic mudstone-halite, and terrigenous clastic sediments. |
Palmer, D.P. | Bureau of Economic Geology |
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Landsat-based lineament analysis, East Texas basin and Sabine uplift area | 1987 | Lineament analysis was used to study the relationship between subsurface structure and surficial features in East Texas, southeastern Oklahoma, southwestern Arkansas, and northwestern Louisiana-areas of low topographic relief, moderate vegetation cover, and diverse land use. |
Baumgardner, R.W., Jr. | Bureau of Economic Geology |