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- W9060998 abstract "The Tuscola anticline, in E.-central Illinois, lies astride the complex LaSalle anticlinal belt and dips steeply westward into the Fairfield basin and gradually eastward into the Murdock syncline. Pleistocene sediments, 50 - 250 ft thick, cover the area. Pennsylvanian sediments cover much of the area, thinning to expose an inlier of Mississippian, Devonian, and Silurian rock north of Tuscola. The basal Cambrian formation, the Mt. Simon Sandstone, is penetrated by only 2 wells. Oil production form the Kimmswick (Trenton) began in 1962. As of Jan. 1, 1968, approximately 30 wells were producing oil. Cumulative oil production as of Jan. 1, 1968, is approximately 94,000 bbl. The potential pay zone is confined to the upper 50 - 100 ft of structure and to the upper 125 ft of the Kimmswick, whose permeability ranges from 0.1 to 2.0 md., averaging 0.6, and whose porosity ranges from 2 to 12%. The low gravity of the Kimmswick oil presents production problems. Oil shows, to date unproductive, are present in Pennsylvanian, Devonian, and Silurian rocks. (12 refs.)" @default.
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- W9060998 date "2018-01-08" @default.
- W9060998 modified "2023-09-26" @default.
- W9060998 title "Geology and Oil Production in the Tuscola Area, Illinois" @default.
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