Abstract:Large areas of offshore Texas remain unexplored even though sedimentary facies and structural traps favor the generation and accumulation of hydrocarbons. Rapid deposition of sand-rich deltaic and Strandline facies that prograded over thick prodelta, shelf, and slope muds caused contemporaneous faulting with displacements up to 10,000 feet. Sandstones thicken substantially on downthrown sides of faults, but shale out a few miles basinward of the ancient shelf margins. These regional expansion faults are slight… Show more
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