Sequence stratigraphy and lithostratigraphy of Devonian reservoir successions, Arkoma Basin, northeastern Oklahoma and northern Arkansas | Posted on:2008-03-08 | Degree:M.S | Type:Thesis | University:University of Arkansas | Candidate:Boyce, Matthew L | Full Text:PDF | GTID:2440390005455309 | Subject:Geology | Abstract/Summary: | | The Devonian System is represented in the northern Arkoma Basin of Arkansas and immediately adjacent Oklahoma by three unconfornity-bounded units designated the Penters Interval, Clifty Formation and Chattanooga Shale, in ascending order. In Arkansas, these units are assigned Lower, Middle and Upper Devonian/Lower Mississippian ages respectively, although biostratigraphic data are uneven. Subsurface analysis of the units indicates that the Penters interval is a pervasive deposit of penecontemporaneous chert and calcisiltites. The Penters can be separated into "Upper" and "Lower" intervals that are divided by a Lower Devonian Shale Marker, which reflects a transgression, maximum flooding and highstand across a siliciclastic, carbonate-rimmed shelf. Chert lithology mirrors that of the lower Boone Formation (Lower Mississippian) suggesting a volcanic source of the silica and deposition below the sediment-water interface, while the calcisiltites were still poorly indurated. The Middle Devonian was a period of mostly erosion that is represented in Arkansas only by the Clifty Formation, a lowstand shoreface deposit. The succeeding transgression during the Upper Devonian is represented by the Sylamore Sandstone, basal member of the Chattanooga Shale. It is a chertarenite with a significant fraction of angular, phosphatic, and chert gravel as well as a small orthoquartizic sand component. The Chattanooga is a dark, black, carbonaceous shale that has pronounced thickening south and east of its outcrop, and a basal contact forming an angular unconformity with earlier strata. | Keywords/Search Tags: | Devonian, Arkansas | | Related items |
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