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- W2034321800 abstract "Numerous small occurrences of Fort Payne oil and gas are found in Kentucky and Tennessee, each difficult to interpret since they seldom fit the structural grain as indicated by other geologic markers. On gamma-ray logs, the reservoir rock is distinctive; it appears in most cases as a porous, clean limestone body interclated between shalier or siltier layers. At the surface, these bodies are very fossiliferous, largely crinoidal, and they resemble biostromes or fossil gardens. These occurrences of more prolific production from the Fort Payne occupy the Cumberland Saddle area of the Cincinnati Arch where pre-Chattanooga erosion has either reduced the Hunton Group rocks to a feather edge or has totally removed them. In the area, the Osage Series is the thick Fort Payne Formation, plus the relatively thin New Providence Shale of the Borden Group below. To the northeast, the Fort Payne is replaced from below by additional and coarser clastics of the Borden Group, which appears to be a deltaic deposit with the beds foreset to the southwest; thus the Fort Payne production appears to lie just seaward from the continental-marine transition zone of the Osage time. (11 refs.)" @default.
- W2034321800 created "2016-06-24" @default.
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- W2034321800 date "1971-01-01" @default.
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- W2034321800 title "Fort Payne production in the Cumberland Saddle area of Kentucky and Tennessee" @default.
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