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- W2034039433 abstract "In north Texas, the Mississippian limestone terrain of the Texas craton was subaerially exposed and diastrophically deformed prior to Pennsylvanian marine transgression. The depositional environments of the Lower Pennsylvanian Bend conglomerates subsequently deposited on this dissected Mississippian surface were exceptionally diverse. In southern Baylor County, these oil productive sandstone bodies are morphologically and stratigraphically similar to both ancient and modern fluvial valley fill. An isopach map of a Bend genetic increment of strata unconformably overlying the Mississippian limestone depicts the paleotopography of the eroded Mississippian terrain as it appeared prior to deposition of the overlying Bend Group. In the study area, anomalous isopach thicks delineate paleovalleys incised into the Mississippian limestone. These sediments thicken at the expense of unconformably underlying Mississippian strata - a diagnostic criterion of valley-fill sediments. Bend conglomerates at the base of these dendritic isopach thicks appear to have been deposited by braided streams within the valleys. These fluvial basal Bend conglomerates serve as structural-stratigraphic oil reservoirs in two one-well fields in southern Baylor County. A paucity of deep well control in the study area, however, makes the risks of exploring for these narrow, sinuous sandstone bodies high." @default.
- W2034039433 created "2016-06-24" @default.
- W2034039433 creator A5029171583 @default.
- W2034039433 date "1986-01-01" @default.
- W2034039433 modified "2023-09-26" @default.
- W2034039433 title "Oil-Productive Basal Pennsylvanian Valley-Fill Sandstones--Southern Baylor County, Texas: ABSTRACT" @default.
- W2034039433 doi "https://doi.org/10.1306/9488570a-1704-11d7-8645000102c1865d" @default.
- W2034039433 hasPublicationYear "1986" @default.
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