Abstract
The Devonian Thirtyone Formation is a prolific producer on the Central Basin Platform in west Texas having produced over 750 MMBBL from chert reservoirs and containing as much as 650 MMBBL remaining reserves. One of the play concepts for this reservoir is laminated beds deposited as turbidites in a deep sea environment. The locations of the lobes and channels and their feeder channels cannot uniquely be determined from well control and 2-D seismic.
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