Possible Origins of the Livingston Fault Zone

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dc.contributor.author Schneeflock, Robert Donald Jr.
dc.date.accessioned 2020-01-15T14:37:11Z
dc.date.available 2020-01-15T14:37:11Z
dc.date.issued 1972
dc.identifier.uri http://ir.ua.edu/handle/123456789/6421
dc.description.abstract The Livingston fault zone is restricted to the outcrop of the Selma Chalk of upper Cretaceous age in Sumter and Marengo Counties, Alabama. This zone is unique among Gulf Coastal Plain structures in that it contains many horsts and grabens which are bounded by reverse faults. These faults dip both to the northeast and southwest and strike North 70 degrees West with a mode for fault plane dip of 40 degrees to 45 degrees.
dc.format.extent 51 pp.
dc.format.mimetype application/pdf
dc.language English
dc.language.iso en_US
dc.publisher University of Alabama Libraries
dc.title Possible Origins of the Livingston Fault Zone en_US
dc.type text
dc.type thesis
etdms.degree.department Geology
etdms.degree.grantor University of Alabama
etdms.degree.level graduate
etdms.degree.level M.S.

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