ABSTRACT
Within the Ham Gossett oil field, Kaufman County, Texas, there is more subsurface control through the entire Cretaceous section than anywhere else along the Mexia-Talco fault zone.
The structure of the eleven reservoirs now producing is largely related to anticlinal closure in the upthrown block against a normal fault. For the first time along the Mexia-Talco fault zone, however, production is also developed on an anticlinal ridge of low relief paralleling the fault in the downthrown block.
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