Sedimentary fills of the Bor Basin (Central Anatolia): Climate and environment during early holocene and the mid-holocene

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dc.contributor.authorGürel, Ali
dc.date.accessioned2024-11-07T10:39:26Z
dc.date.available2024-11-07T10:39:26Z
dc.date.issued2016
dc.departmentNiğde Ömer Halisdemir Üniversitesi
dc.description16th International Multidisciplinary Scientific GeoConference: SGEM 2016 -- 30 June 2016 through 6 July 2016 -- Albena -- 124231
dc.description.abstractHolocene alluvial and lacustrine deposits characterize the so-called Quatrnary fills of the Bor Basin (central Turkey) and consist of conglomerate, sandstone, mudstone, limestone, and paleosol-calcrete units. To understand the any climate changes hidden in sedimentary rocks and paleosols and pedogenic processes mentioned above, it is planned to perform XRD (X ray diffraction), SEM (Scanning Electron Microscope), XRF (X-Ray Fluorescence) and stable isotope element analysis due to determine for the analysis of geochemical, mineralogical sedimentogical compositions. During the Late Glacial, a shallow freshwater lacustrine phases and paleosols are identified from 40 000 to 11 000 yr BP. The Holocene environmental evolution shows a period of paleosols, marsh or shallow lake sedimentation from 6 000 to 5 500 yr BP. This period is interrupted by second drought period and this corresponds to calcareous rich mudstones in the area. This is covered during the Late Holocene by the renewal of marshes, shallow lake sediments and paleosols. The temperature increase during the last period, uprising and closed basin structure, salinization started taking place and the process still continues due to palaeoclimatical changes. © SGEM2016.
dc.identifier.doi10.5593/SGEM2016/B11/S01.067
dc.identifier.endpage540
dc.identifier.isbn978-619710555-1978-619710558-2978-619710561-2978-619710563-6978-619710565-0978-619710568-1978-619710555-1
dc.identifier.issn1314-2704
dc.identifier.scopus2-s2.0-84994180835
dc.identifier.scopusqualityN/A
dc.identifier.startpage533
dc.identifier.urihttps://doi.org/10.5593/SGEM2016/B11/S01.067
dc.identifier.urihttps://hdl.handle.net/11480/10957
dc.identifier.volume1
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherInternational Multidisciplinary Scientific Geoconference
dc.relation.ispartofInternational Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_20241106
dc.subjectBor Basin
dc.subjectCentral Anatolia
dc.subjectHolocene
dc.subjectLacustrine Sediments
dc.subjectMineralogical-geochemical content
dc.titleSedimentary fills of the Bor Basin (Central Anatolia): Climate and environment during early holocene and the mid-holocene
dc.typeConference Object

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