Abstract
Data are presented indicating that: (1) the Yates sand horizon of eastern Pecos County is correlated very definitely with the Queen sand horizon of New Mexico; (2) the anhydrite section below the base of the salt, on the eastern rim of the Central Basin platform, changes to limestone at the western margin of the platform; (3) the San Andres formation in the Artesia field of New Mexico is correlated with the lower part of the Delaware sandstone.
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