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- W2079882359 abstract "The unconsolidated terrestrial sediments in central-western Texas consist of a Pliocene wedge truncated eastward, discontinuous remnants of three pre-Wisconsin interglacial stages, and Wisconsin to Recent terrace deposits and wind-blown sand. This material very occasionally rests on siliceous conglomerate of Oligocene or Miocene age. Distinctive units can be traced from the Llano Estacado (High Plains) onto outliers east of them and across the extensive upland plains of north-central Texas. Most important is the unique algal limestone, which constitutes the upper cap rock of the High Plains and extends more than 100 miles farther east. It is part of a soil profile developed on limestone gravel, apparently of Sangamon interglacial age. The region's most extensive topographic surface, developed almost on top of the algal limestone, continues into a pediment on Cretaceous limestone, which was a source of gravel. This and other altered limestone gravels are the caliche of the region. The terrestrial sediments were deposited while sea level was relatively high. At such times erosion, characterized by pedimentation with retreating scarps, gave way to widespread alluvia-tion. In the Pleistocene this alluviation occurred during the interglacial stages. The Pliocene and Oligocene-Miocene beds also are correlated tentatively with marine transgressions recorded in Gulf Coast sediments and with basin-filling in the eastern part of the Rocky Mountains. These sediments affect the petroleum industry by the limitations they impose on surface-exploration techniques." @default.
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- W2079882359 date "1957-01-01" @default.
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- W2079882359 title "Cenozoic Strata on the Southwestern Osage Plains of Texas" @default.
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- W2079882359 doi "https://doi.org/10.1086/626405" @default.
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