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- W321263423 abstract "Data from four drill holes and other subsurface data were compiled to analyze for possible offset on a suspected fault near an earthquake epicenter in the New Madrid seismotectonic area of western Kentucky. The drill holes penetrated unconsolidated Eocene and younger sediments of the Mississippi Embayment. These holes were located along an east to west line that intersected the northeast trending lineament of the suspected fault. Lignite was encountered in each of the drill holes. Correlation of lignitic layers, geophysical logs, and drill cuttings suggests that the lignite was deposited on a gently rolling, westward-dipping surface. This surface dips westward at approximately 23 feet per mile. The underlying Wilcox Formation is reported to dip westward at 23 feet per mile. No evidence was found to support the presence of offset on the suspected fault, but the inability to correlate the lignitic deposits unequivocally made it impossible to rule out the possibility of a fault. Furthermore, the similarity between the dip of the Wilcox Formation and the dip of the lignite horizon suggests no offset along the line of the drill holes. Five possibilities about the occurrence of a fault in the area investigated are: (1) no offset due to faultingmore » exists, (2) the suspected fault was not intersected by the line of drill holes presented in this report, (3) the presence of unconsolidated deposits may have dampened effects of faulting, (4) offset due to faulting exists but is too small to detect, and (5) offset on the lineament occur only to the south and died out before reaching the study area.« less" @default.
- W321263423 created "2016-06-24" @default.
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- W321263423 date "1982-09-01" @default.
- W321263423 modified "2023-09-27" @default.
- W321263423 title "Correlation of lignite beds for fault identification in the Mississippi Embayment area of western Kentucky. Final report" @default.
- W321263423 hasPublicationYear "1982" @default.
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