Upper Cretaceous chalk reservoir with selective oil production across Mississippi
Get a Free Mineral ValuationThe Selma Chalk is an Upper Cretaceous-age carbonate that produces oil from selected Mississippi fields at depths of approximately 6,000-10,000 ft TVD. The Selma is the Mississippi equivalent of the Austin Chalk in central Texas — a fractured chalk reservoir where production depends on natural fracture density. Active Mississippi Selma Chalk positions exist in selected counties across the central producing belt.
Mineral interests on Selma Chalk — Mississippi-producing acreage are typically inherited multiple generations deep. The valuation framework depends on the specific reservoir's depth, decline rate, and the operator's maintenance posture. For broader context see our Mississippi CO2 Floods Overview.
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