Abstract

The Smackover Formation is an Upper Jurassic (Oxfordian) carbonate sequence found entirely in the subsurface throughout the northern Gulf of Mexico region. The Upper Smackover consists of oolitic and associated grainstones that have become known as prolific hydrocarbon reservoirs during the last four decades.KeywordsPetroleum GeologistDolomite CrystalPlane LightOolitic GrainstoneSalt TectonicsThese keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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