Upper Tertiary and Quaternary depositional systems, central Coastal Plain, Texas : regional geology of the coastal aquifer and potential liquid-waste repositories

dc.coverage.spatialGulf Coast Plain, Texas
dc.creatorSolís I., Raúl Fernando
dc.descriptionTo obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0108.
dc.description.abstractUpper 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. These sedimentary units constitute the last major depositional episodes in the northwestern Gulf Coast Basin. Late Miocene deposition is represented by transgressive shelf and shallow-marine shales overlain by progradational clastics of the upper part of the Lower Fleming, Upper Fleming, and Lower Goliad-Willis units. Aminor Pliocene transgressive event is represented by downdip marine embayment facies of the Upper Goliad-Willis unit. Finally, Pleistocene highstand fluviodeltaic progradation (Lissie and Beaumont units) terminated pre-Holocene sedimentation. Interpretation of sediment distribution, established by constructing a series of net- and percentage-sand maps for each unit, permits delineation of the following main depositional systems: fluvial braided-meanderbelt and floodbasin; fluvio-deltaic systems; lagoon; large marine embayments; small bayhead deltas; thick wave-dominated deltas; strandplain; and thick, stacked coastal barriers. Western fluviodeltaic systems were consistently less active than the eastern ones, which deposited greater volumes of sand. Inherited, subtle structural influence of the deeper seated San Marcos Arch had some effect on sediment distribution and paleogradients. Shallow extensions of the deeper Vicksburg, Frio, and Miocene fault systems display respectively decreasing (from 400 ft, 122 m) displacements in the section studied. Faults clearly played a central role in the distribution of fluvial, deltaic, and strike-oriented coastal sands. Most sands in the updip parts of the operational units contain fresh water, whereas those of downdip areas contain predominantly brackish to saline waters. The area with greatest reservoir potential for fresh water includes Victoria, Jackson, Wharton, and Colorado Counties. Possible use of sealed, thick coastal sands in the Lower Fleming unit for the disposal of industrial and municipal liquid waste is recommended.
dc.description.departmentUT Libraries
dc.description.departmentBureau of Economic Geology
dc.format.dimensionsiv, 89 p. : ill. ; 28 cm.
dc.publisherUniversity of Texas at Austin. Bureau of Economic Geology
dc.relation.ispartofVirtual Landscapes of Texas
dc.relation.ispartofReport of Investigations
dc.relation.ispartofseriesReport of Investigations (University of Texas at Austin. Bureau of Economic Geology), no. 108
dc.subjectAquifers -- Texas -- Gulf Region
dc.subjectGeology, Stratigraphic -- Quaternary
dc.subjectGeology -- Stratigraphic -- Tertiary
dc.titleUpper Tertiary and Quaternary depositional systems, central Coastal Plain, Texas : regional geology of the coastal aquifer and potential liquid-waste repositories

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