HYDROCARBON POTENTIAL OF THE LOWER SMACKOVER FORMATION IN ARKANSAS, LOUISIANA, AND MISSISSIPPI
This study offers a new depositional system and sequence stratigraphic framework of the Smackover Formation and evaluates the hydrocarbon potential of its Lower Member. According to this synthesis, the Smackover Formation consists of four sequences which were deposited in a strongly progradational depositional system. From the oldest to the youngest, they are here referred to as Smackover Sequence-1 (SS-1) to Smackover Sequence-4 (SS-4).
The SS-1 and SS-2 were deposited in the inner shelf region. These two sequences do not posses the laminated lime mudstone and the Brown Dense Limestone lithofacies, have thin ooid grainstone layers, were influenced by microbial processes, their original mineralogy was aragonitic, and were exposed to extensive meteoric diagenesis.
SS-3 and SS-4 formed in the middle shelf to basinal areas. These two sequences have well-developed laminated lime mudstone and the Brown Dense Limestone which are rich in organic carbon, have turbidite-derived sandstones, and occasionally dolomitized. The ooid grainstone lithofacie of these two sequences are thick and were deposited as prograding shelf margin marine shoals.