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dc.creatorHatley, Allen Grady
dc.date.available2011-02-18T21:34:47Z
dc.date.issued1955-05
dc.identifier.urihttp://hdl.handle.net/2346/16488en_US
dc.description.abstractMicropaleontologic and lithologic data obtained from several exposures of Finlay, Duck Creek and Fort Worth equivalents are recorded for comparison with similar information from other areas. Biostratigraphic and paleoecologlcal inferences have been made. Evidence obtained from ostracodes and foraminifera indicates that a Finlay equivalent, not Kiamichi, is present north of Kent. There is a lack of information on the Fredericksburg-Washita contact as it is not exposed within the area studied. For the most part the Duck Creek and Fort Worth equivalents were deposited in a sea of normal marine environment with depths of 5 to 60 fathoms, the only exception being in the upper portion of the Duck Creek equivalent whZere evidence indicates a slight restriction and possible regression of the sea.
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherTexas Tech Universityen_US
dc.subjectStratigraphic -- Cretaceousen_US
dc.subjectGeologyen_US
dc.subjectGeology -- Texasen_US
dc.titleMicropaleontology of a part of the Lower Cretaceous in Kent Quandrangle, Texas
dc.typeThesis
thesis.degree.nameM.S.
thesis.degree.levelMasters
thesis.degree.disciplineGeology
thesis.degree.grantorTexas Tech University
thesis.degree.departmentGeology
thesis.degree.departmentGeosciences
dc.degree.departmentGeologyen_US
dc.rights.availabilityUnrestricted.


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