Paleogeography and Cementation in a Mississippian Oolite Shoal Complex: Ste. Genevieve Formation, Willow Hill Field, Southern Illinois Basin
Published:January 01, 1993
Ronald D. Manley, P. W. Choquette, M. B. Rosa, 1993. "Paleogeography and Cementation in a Mississippian Oolite Shoal Complex: Ste. Genevieve Formation, Willow Hill Field, Southern Illinois Basin", Mississippian Oolites and Modern Analogs, Brian D. Keith, Charles W. Zuppann
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Lenticular bodies of porous, permeable ooid grains tone in the upper Ste. Genevieve Formation (Valmeyeran, middle Mississippian) form small oil reservoirs in Willow Hill field, Jasper County, Illinois. The ooid grainstones occur in a swarm of elongate, convex-upward bodies 0.2-2.5 mi (0.32-4.0 km) long by 500-3000 ft (150-1000 m) across and up to 15 ft (5 m) thick. They are interpreted as largely marine shoal deposits that developed along a bioclastic carbonate-sand shoal of low relief and NW-SE trend. Some show evidence of exposure and residence of freshwater lenses. Lime mudstones form capping and updip seals.
Early cements, mainly meteoric in origin, prevented physical compaction and "propped" original pores. Fringing isopachous cements, interpreted as phreatic, resulted in systems of well-connected pores. Ooid grainstones with this combination of cements have porosities (ϕ) of 6.0-17.2% (average 12.7%) and permeabilities (k) of <0.1-228 md (average 113 md). In other ooid grainstones, meniscuslike cements (vadose) also propped original pores, but were overgrown by later blocky burial cement that resulted in less well-connected pores and poor to non-reservoir facies with (|)s of 5.2-17.9% (average 12.8%) but ks of <0.1-1.0 md, with an average of 0.13 md. In associated bioclastic grainstones, ϕ and k values are somewhat less than those of the reservoir-quality ooid grainstones due to syntaxial cement around uncoated crinoid grains.
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Mississippian Oolites and Modern Analogs
A coincidence of tectonic, eustatic, and geochemical conditions resulted in substantial deposits of oolitic limestone during later Mississippian time in the continental United States. These oolitic limestones have formed petroleum reservoirs with favorable primary and secondary recovery characteristics. Significant potential reserves in stratigraphic traps remain to be discovered and developed in these reservoirs.