Devonian-Mississippian Transition in Central Texas
Reprinted from Geological Society of America Bulletin, v. 68, no. 7, 1957. From the Abstract:The Devonian-Mississippian transition outcrops of central Texas are here described summarily and assigned to a new stratigraphic unit, the Houy Formation. The beds included are mainly Upper Devonian, but partly Lower Mississippian. Locally a basal fraction may be Middle Devonian. Although the deposits included are diverse and their associations complex, the maximum surface thickness so far known is only about 17 feet. The principal subdivisions, in their usual ascending order, are the Ives Breccia Member (Plummer in Bullard and Plummer, 1939), the Doublehorn Shale Member (new), and a thin unnamed phosphoritic interval. Commonly, however, one or more of these members is absent, and rocks not assigned to any member are present. The Ives Breccia Member includes lag deposits of detrital chert of varied age and source. The Doublehorn Shale Member includes black, fissile, spore-bearing shale of Late Devonian age which in a few exposures grades upward into shale of Early Mississippian age. The phosphatic beds are partly Late Devonian and partly Early Mississippian. Remnants of the Doublehorn Shale Member have been found only along the eastern side of the Llano region, but the other units are more widely distributed, and rocks assignable to the Houy Formation are to be looked for between Ordovician and Upper Mississippian deposits anywhere around the Llano region.
Cloud, P. E., Barnes, V. E., and Hass, W. H., 1957, Devonian-Mississippian Transition in Central Texas: The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations No. 31, 10 p.
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The University of Texas at Austin, Bureau of Economic Geology
Report of Investigation