The Pennsylvanian Lower Strawn Group, Jack and Wise Counties, Fort Worth Basin : facies distribution and stratigraphic architecture

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2020-05-08

Authors

Roberts, Andrew Kearny

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Abstract

The Lower Strawn Group in Jack and Wise counties of the Fort Worth Basin are laterally and vertically heterogeneous deltaic deposits comprising sandstones, siltstones, and shales with thin, discontinuous carbonates and coal seams reflecting variable icehouse condition controls. Given a general lack of differentiation of individual sequences in the Lower Strawn in Jack and Wise counties, this study develops a stratigraphic framework, highlights relationships between component facies of the Lower Strawn, establishes individual sequences, and identifies depositional controls and their effects on reservoir predictability. With an estimated 38 million barrels of oil (MMBO) & 56 billion cubic feet of gas (BCF) of mean total undiscovered resources located in Pennsylvanian/Permian fluvio-deltaic sandstones and conglomerates, analogous to depositional environments in many foreland basins globally, this study provides a key dataset with respect to component depositional facies and reservoir architecture for more informed resource assessment. Based on core description and interpretation, depositional environments of the Lower Strawn Group include prodelta, medial delta front, interdistributary-bay, channel mouth bar, and distributary-channel deposits. These interpreted depositional environments, their well-log pattern, and vertical facies relationships enable an interpretation that fluvio-deltaic depositional systems dominated in the Lower Strawn Group. Wireline log correlations of regionally-extensive maximum flooding surfaces were used to develop a sequence stratigraphic framework that identified eleven regressive-transgressive, fluvio-deltaic sequences averaging 90-240ft thick, collectively spanning a thickness of 1,000-2,700 ft. (305-823 m.) as the interval onlapped the forebulge of the Fort Worth Foreland Basin. A south-southwest overall direction of progradation was identified based on the distribution of net sandstone thickness trends. The depocenters contained within these sequences reflect similar geometries to those described from fluvio-deltaic systems of the Mississippi River and Yukon River Deltas. With elevated porosity trends found to be associated with homogeneous channel-mouth bar and distributary-channel deposits, a better understanding of internal reservoir characteristics and distribution helps improve predictability for operators pursuing complex stratigraphy containing hydrocarbon resources in similar depositional settings.

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