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Sedimentology and diagenesis of the basinal facies of the Dimple Limestone, Marathon Basin, West Texas
(Texas Tech University, 1985-05)
The Dimple Limestone (Morrowan?-Atokan), Marathon Basin, Texas, represents a break in the Ouachita clastic flysch sequence. Carbonate material was transported from the present northwest into the Ouachita trough, an abrupt ...