Clay Minerals in Atokan Deep-Water Sandstone Facies, Arkoma Basin: Origins and Influence on Diagenesis and Reservoir Quality
Published:January 01, 1992
David W. Houseknecht, Louis M. Ross, Jr., 1992. "Clay Minerals in Atokan Deep-Water Sandstone Facies, Arkoma Basin: Origins and Influence on Diagenesis and Reservoir Quality", Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones, David W. Houseknecht, Edward D. Pittman
Download citation file:
Strata of the lower and middle Atoka Formation in the Arkoma Basin comprise submarine-fan and marine-slope facies that display a variety of primary and secondary sedimentary structures, formed by sediment gravity-flow depositional processes and dewatering, respectively. Primary sedimentary structures are most common in beds deposited by unconfined sediment gravity flows on submarine-fan lobes, whereas secondary sedimentary structures are most common in beds deposited by channelized sediment gravity flows in fan channels and slope channels. Primary sedimentary structures display horizontal fabrics, whereas secondary sedimentary structures display deformed and vertical fabrics. Abundance and distribution of clay minerals in Atoka sandstones are related to sedimentary structures. Beds that display primary sedimentary structures contain little detrital clay that is sparsely disseminated through the sandstone. In contrast, beds that display secondary sedimentary structures contain more detrital clay that forms pervasive grain coatings, bridges between grains, and consolidation laminae. Other beds lack sedimentary structures and display abundant detrital clay that forms a matrix-supported fabric.
The abundance and distribution of detrital-clay minerals exerted significant influences on diagenesis and reservoir quality of Atoka sandstones. Among sandstones with grain-supported fabrics, those that display primary sedimentary structures and contain little detrita) clay were pervasively cemented by quartz overgrowths and are characterized by poor reservoir quality. Those that display secondary sedimentary structures and contain more abundant detrital clay retained primary porosity because quartz-overgrowth nucleation was inhibited by clay coatings on detrital grains. Porosity was enhanced in these sandstones by dissolution of framework grains, and the sandstones are characterized by good reservoir quality. Sandstones with matrix-supported fabrics apparently had little original porosity, which was reduced by compaction of the pervasive matrix; they are characterized by poor reservoir quality. These observations suggest that channelized turbidite facies have greater potential to retain good reservoir quality than unconfined turbidite facies, because the former have detrital-clay minerals emplaced within sand during dewatering and those clay minerals inhibit destruction of porosity by quartz cementation.
Figures & Tables
Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones
Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstone–This volume grew out of a symposium held at the 27th Annual Meeting of the Clay Minerals Society in Columbia, Missouri on October, 1990. The symposium was designed to present a current synthesis of research devoted to the origin, diagenesis and petrophysics of clay minerals in sandstones. International authors demonstrate a multidisciplinary approach to interpreting the origin and diagenesis of clay minerals in sandstones and to evaluating their influence on reservoir quality. This volume bridges a gap between petrographic and geochemical researchers and reservoir geologists and engineers.