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dc.contributor.advisorErten, Hasan N.
dc.contributor.authorTadjiki, Soheyl
dc.date.accessioned2016-01-08T20:10:10Z
dc.date.available2016-01-08T20:10:10Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/11693/17423
dc.descriptionAnkara : Department of Chemistry and Institute of Engineering and Sciences, Bilkent Univ., 1992.en_US
dc.descriptionThesis (Master's) -- Bilkent University, 1992.en_US
dc.descriptionIncludes bibliographical references leaves 73-78en_US
dc.description.abstractThe and profiles are determined at two locations in southern coast of Spain, Three locations in southern coast of Turkey and two locations in coast of Cyprus. Compaction-corrected sedimentation rates are derived for all locations using data. The rates range from 1..39± 0.12 crn.y"' (0.50±0.04 g.cm“^.y“^) to 0.08±0.01 cm.y“^ (0.039±0.003 g.cm~'^.y“^) (0.50±0.04g.cm"^.y~^). Except for BC-6A, for all of the locations the ^^’^Cs profile is used to compute sedimentation rates which are in a good agreement with those of '^^°Pb method. The result of the Constant Initial Concentration and Constant Rate of Supply dating models are in a good agreement with each other whereas in BC-6A and KS-1 cores only Constant Rate of Supply model is valid to calculate sedimentation rate. The flux of unsupported '^^°Pb vary between 0.74±0.01 pCi.cm“^ and 0.11 ±0.03 pCi.cm“^. The average depositional flux is found to be considerably low in the coast of Turkey and Cyprus, whereas it is found to be high in the coast of Spain.en_US
dc.description.statementofresponsibilityTadjiki, Soheylen_US
dc.format.extentix, 78 leavesen_US
dc.language.isoEnglishen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subject210 Pben_US
dc.subject137 Csen_US
dc.subjectSedimentation rateen_US
dc.subjectCs profileen_US
dc.subjectConstant Initialen_US
dc.subjectConstant Rate of Supply modelen_US
dc.subjectThe flux of unsupported 210 pben_US
dc.subjectConcentration modelen_US
dc.subject.lccQD501 .T34 1992en_US
dc.subject.lcshSedimentation analysis.en_US
dc.titleRadiochronology of sediments from various regions of the Mediterranean Sea by direct gamma spectroscopy using natural 210Pb, 226Ra and fallout 137Csen_US
dc.typeThesisen_US
dc.departmentDepartment of Chemistryen_US
dc.publisherBilkent Universityen_US
dc.description.degreeM.S.en_US


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