|Name||Santa Anna Branch Shale and Sedwick and Moran Formations, undivided|
|Geologic age||Permian; Wolfcamp Series|
Sedimentary > Clastic > Mixed-clastic > Siltstone-mudstone (Bed)
Sedimentary > Clastic > Mixed-clastic > Sandstone-mudstone (Bed)
Sedimentary > Carbonate > Limestone (Bed)
|Comments||Mudstone, shale, and sandstone. Mostly mudst. and shale, gray, tan, maroon, thick beds, colors intertongue locally; a few thin ss lentils and sheets, v fine grained, calcar. Limestone lt-gray, fine-grained, thin bedded, nodular, weathers to hard slabs and blocks, thickness 1-3 ft. Sandst. brown, med-grained, large-scale crossbeds thickness 8-10 ft. Thickness of Santa Anna Branch Shale 170-190 ft., Sedwick Fm 30-40, Moran Fm 160-210|
Bureau of Economic Geology, 1987, Wichita Falls-Lawton Sheet, Geologic Atlas of Texas: University of Texas at Austin, Bureau of Economic Geology, scale 1:250,000.
Bureau of Economic Geology, 1992, Geologic Map of Texas: University of Texas at Austin, Virgil E. Barnes, project supervisor, Hartmann, B.M. and Scranton, D.F., cartography, scale 1:500,000.
|Counties||Brown - Coleman - Concho - McCulloch|