“…Sedimentary rocks reach a maximum combined thickness of between 14,000 and 20,000 feet in the Raton basin (Baltz, 1965;Roberts and others, 1976) and 12,700 feet in the Las Vegas basin (Baltz, 1965). The sedimentary section in these basins is largely comprised of Pennsylvanian (about 5,500 feet maximum, Baltz, 1965;Roberts and others, 1976), Permian (about 2,000 feet maximum, Dixon, 1967;Roberts and others, 1976), Cretaceous (4,100 feet maximum, Molenaar, 1983), and Tertiary (5,000 feet maximum, Speer, 1976) rocks. The Pennsylvanian and Lower Permian rocks in the Rowe-Mora basin consist of dark basinal shale in the lower part of the Pennsylvanian System (Morrowan, Atokan, lower Desmoinesian) which are flanked on the west by nonmarine arkosic sandstones and on the east by shelf carbonate rocks (Roberts and others, 1976;Casey, 1980) whereas the upper part of the Pennsylvanian System and the lower part of the Permian System (Wolfcampian) are represented by nearshore carbonate rocks flanked on the north, west, and east by arkosic sandstone and conglomerate (Roberts and others, 1976).…”