Abstract

The sedimentary sequence and facies changes in the subsurface of the Panhandle of Texas are shown by three cross-sections. The stratigraphic column is divided into 13 geologic subdivisions. A paleogeo-logic map presents the areal distribution of each geologic subdivision. On each map parallel lines slanted to right indicate presence of sediments and those slanted to left indicate their absence. The effects of orogenic and epeirogenic movements are discussed.

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