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Paleocurrents, trace fossils, and facies analysis of a vertical profile through a terrigenous clastic sequence are combined to determine the paleogeography for a part of the Lower Mississippian.
A lithic description and gamma-ray log of a classic outcrop section provide a basis for correlation with subsurface units.
A redefinition of the Holtsclaw siltstone member and a review of the stratigraphic relations brought out by geologic mapping.
Includes entries for maps and atlases.