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    A study of Quaternary active tectonics

    Abousaif, Alzubair
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    [PDF] public.pdf.pdf (2.407Kb)
    [PDF] research.pdf.pdf (4.462Mb)
    [PDF] Short.pdf.pdf (3.969Kb)
    Date
    2012
    Format
    Thesis
    Metadata
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    Abstract
    [ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] This study presents first results on the topographic survey and shallow seismic reflection profile to assess Quaternary faulting in the northwestern Wind River Basin, Wyoming. Degradation model suggests too old fault scarp ages comparing them with estimated correlation ages, which leads to the conclusion that these scarps are fold scarps, and this kind of scarp folding interpreted as monocline. Interpretation of a break in reflection dipping toward the north is a high angle reverse fault. Therefore, the surface expression of the monocline formed as result of subsurface fault displacement.
    URI
    http://hdl.handle.net/10355/33256
    Degree
    M.S.
    Thesis Department
    Geological sciences (MU)
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    Access to files is limited to the University of Missouri--Columbia.
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    • 2012 MU theses - Access restricted to MU
    • Geological Sciences electronic theses and dissertations (MU)

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