--> Abstract: Structure and Evolution of North Choctaw Ridge Field, Alabama, a SaltRelated Footwall Uplift Along the Peripheral Fault System, Gulf Coast Basin, by J. Qi, J. C. Pashin, and R. H. Groshong, Jr.; #90932 (1998).
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Abstract: Structure and Evolution of North Choctaw Ridge Field, Alabama, a SaltRelated Footwall Previous HitUpliftNext Hit Along the Peripheral Fault System, Gulf Coast Basin

QI, J.
The University of Alabama, Tuscaloosa, AL;
J. C. PASHIN
Geological Survey of Alabama, Tuscaloosa, AL;
R. H. GROSHONG, Jr.
The University of Alabama, Tuscaloosa

North Choctaw Ridge (NCR) Field is a structural trap producing from the Jurassic Smackover Formation which is in the Gilbertown graben system, at the updip limit of the Louann Previous HitSaltNext Hit. The field is in the footwall Previous HitupliftNext Hit below of one of the faults forming the northern boundary of the graben system. The top seal is anhydrite in the overlying Buckner Formation, and the boundary fault provides a lateral seal. The 325-acre field has produced 8.1 million barrels of oil and 4.2 tcf of gas since its discovery in 1972. The geometry and evolution of the structure has been determined from a threedimensional Previous HitinterpretationNext Hit of the graben system and from a balanced and sequentially restorable cross section derived from it. A graph of graben area versus depth shows that the cross section is both area and length balanced with a lower detachment near the base of the Louann Previous HitSaltNext Hit. The graph further indicates that significant structural growth began in Early Cretaceous time. During Early Cretaceous extension, three major southdipping, down-to-the-Gulf faults formed, creating an imbricate system of half grabens (the Melvin fault system) with NCR Field being a Previous HitsaltNext Hit-cored Previous HitupliftNext Hit beneath the southern fault (Melvin C). Subsidence south of the Melvin fault system indicates contemporaneous Previous HitsaltNext Hit deflation, but the area-depth relationship suggests that the NCR Field was simultaneously uplifted above regional dip, presumably by inflow of Previous HitsaltTop. The north-dipping boundary fault of the Gilbertown graben system (East Gilbertown fault) developed only after the Lower Cretaceous. Continuing extension produced a full graben between the East Gilbertown and Melvin C faults.

AAPG Search and Discovery Article #90932©1998 GCAGS/GCS-SEPM Meeting, Corpus Christi, Texas