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The document summarizes research on overpressured sandstone bodies encased in mudstone. It presents a model showing how differential sediment loading as a sandstone dips can drive fluid flow into the base and expel it from the crest. The model predicts the spatial variation in pressure within the sandstone and surrounding mudstone. Field observations from two reservoirs are presented that support flow focusing along reservoir sandstones driven by overpressure in the enclosing mudstones. This flow regulates

Author

Aiwarikiaar

Language

EN