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- W1990676906 abstract "Wilburton field is a multizone reservoir on the southwestern edge of the Arkoma basin. The most recent zone to be declared commercial is the Cambrian-Ordovician Arbuckle Group. Faults, structural position, depositional environment, and diagenetic alterations play a role in controlling reservoir quality, communication of fluids and pressures within the reservoir, and stratigraphic correlations. The Arbuckle Group in Wilburton field consists of dolomite, calcareous dolomite and minor clastic-rich intervals, chert, and dolomitic limestones. Early diagenesis consisted of pervasive dolomitization that created a dolomudstone with low (12%) intercrystalline porosity. The regionally extensive Middle Ordovician unconformity, which occurs at the top of the Arbuckle Group, exposed that carbonate surface to meteoric conditions that resulted in formation of karst. The porosity development or enhancement associated with karsting modified depositional textures and their related pore geometries. Stratigraphically, the Arbuckle section can be divided into two zones. An upper zone, 200-250 ft thick, is characterized by a lack of fracturing and brecciation, and by fluid flow mainly through the matrix or intercrystalline pore system. Porosity development in these intervals extends across the field. The lower zone is characterized by multiple intervals of fracturing, brecciation (all three types), and solution collapse. The Arbuckle is most likely productivemore » where solution has enhanced intercrystalline, fracture, and breccia porosity, and burial cements have failed to completely fill pore space. The authors anticipate that porosity development in Arbuckle carbonates in other areas is similarly controlled and should be productive.« less" @default.
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- W1990676906 date "1992-01-01" @default.
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- W1990676906 title "Karst-Related Diagenesis and Reservoir Development in the Arbuckle Group, Wilburton Field, Oklahoma" @default.
- W1990676906 doi "https://doi.org/10.1306/f4c8f5de-1712-11d7-8645000102c1865d" @default.
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