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dc.creatorWells, Neil A.en_US
dc.creatorCoogan, Alan H.en_US
dc.creatorMajoras, Judy J.en_US
dc.date.accessioned2006-07-07T17:57:38Z
dc.date.available2006-07-07T17:57:38Z
dc.date.issued1991-03en_US
dc.identifier.citationThe Ohio Journal of Science. v91, n1 (March, 1991), 35-48en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23428
dc.descriptionAuthor Institution: Department of Geology, Kent State Universityen_US
dc.description.abstractSynsedimentary slumps of Berea Sandstone and diapirs of Cleveland and Bedford Shales are seen in complex delta-front facies at Elyria, Lorain County, OH. Analysis of orientations of fractures, bedding, and crossbeds helps interpret the history of deformation. In many instances, initial conjugate shears formed with least stress parallel to paleoflow, down the paleoslope. Some conjugate joints subsequently become normal and strike-slip faults. Some blocks of Berea show tilting and/or sliding to the extent of creating recumbent overturned drag folds in subjacent shales. Deformation of slide bases varies from brittle to plastic (fluidized). These features support the view that irregular thicknesses of Berea Sandstone are the result of deformation and are not fillings of deep valleys eroded in a Red Bedford delta. We suggest that the Berea represents rapid progradation of sands over formerly deep-water shales following rebound at the end of foreland-basin subsidence.en_US
dc.format.extent3529983 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleField Guide to Berea Sandstone Outcrops in the Black River Valley at Elyria, Ohio: Slumps, Slides, Mud Diapirs, and Associated Fracturing in Mississippian Delta Depositsen_US


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