Abstract
Coral reefs of Oligocene age occur around the salt domes of the Coastal Plain of Texas. The reefs around two domes, Damon Mound and West Columbia, are given in detail with cross-sections of the reefs showing position around the domes. Several interesting facts relative to the movements of the salt plugs are given.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.