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Sedimentary properties of the middle-upper eocene formations in çardak, burdur and incesu, SW Turkey

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dc.contributor.author Toker, Ezher
dc.contributor.author Serkan Akkiraz, M.
dc.contributor.author Yaǧmurlu, F.
dc.contributor.author Akgün, F.
dc.contributor.author Örçen, S.
dc.date.accessioned 2019-08-16T12:44:57Z
dc.date.available 2019-08-16T12:44:57Z
dc.date.issued 2012
dc.identifier.issn 13000985 (ISSN)
dc.identifier.uri http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/8685
dc.description.abstract The integration of sedimentological, palynological and palaeontological data in three dif erent outcrops in SW Turkey provides a clearer understanding of the palaeoenvironments in an area between the Çardak-Dazki{dotless}ri{dotless} Basin and the Isparta region during the Middle-Late Eocene. In this study, the Çardak-Dazki{dotless}ri{dotless} (Başçeşme Formation), Burdur (Varsakyayla Formation) and Isparta (Kayi{dotless}köy Formation) areas have been studied for facies and facies associations. These formations contain alluvial fan, fan delta, shelf and related marine deposits. Detailed field observations allowed 34 lithofacies and 10 facies associations to be identified. The palynomorph assemblages in the Başçeşme and Varsakyayla formations contain biostratigraphically important taxa such as Aglaoreidia cyclops, Triatriopollenites excelsus, Plicatopollis lunatus, Subtriporopollenites constans and Subtriporopollenites anulatus ssp. nanus. The mangrove and back mangrove elements such as Psilatricolporites crassus and Spinizoncolpites sp. also occur in these palynomorph assemblages. The upper parts of the Başçeşme and Varsakyayla formations, which of en exhibit reef developments, contain an assemblage of orthophragmines (Discocyclina sp.), nummulitids (Nummulites sp., Assilina sp., Heterostegina sp., Operculina sp.) and other benthic taxa (Halkyardia sp., Fabiania sp., Asterigerina sp., and Sphaerogypsina sp.). These assemblages indicate shallow benthic zones 18-20 (SBZ 18-20). The absence of foraminifera in the Kayi{dotless}köy Formation does not allow a precise age of the unit to be determined. However, the occurrence of some planktonic foraminifera (Globigerinidae) and the presence of clastic sediments suggest a marine environment with turbidity currents. The lateral and vertical relations of the Başçeşme, Varsakyayla and Kayi{dotless}köy formations suggest a marine transgression from west to east in SW Anatolia during the late Middle Eocene-Late Eocene. © TÜBİTAK.
dc.language.iso English; Turkish
dc.relation.isversionof 10.3906/yer-0909-8
dc.rights info:eu-repo/semantics/closedAccess
dc.subject Benthic foraminifera
dc.subject Eocene deposits
dc.subject Facies analysis
dc.subject Palynology
dc.subject Western taurides
dc.subject benthic foraminifera
dc.subject biostratigraphy
dc.subject Eocene
dc.subject facies analysis
dc.subject lithofacies
dc.subject paleoenvironment
dc.subject paleontology
dc.subject palynology
dc.subject planktonic foraminifera
dc.subject sedimentary structure
dc.subject sedimentology
dc.subject transgression
dc.subject Burdur [Turkey]
dc.subject Denizli [Turkey]
dc.subject Isparta [Turkey]
dc.subject Taurides
dc.subject Turkey
dc.subject Assilina
dc.subject Asterigerina
dc.subject Discocyclina
dc.subject Foraminifera
dc.subject Globigerinidae
dc.subject Heterostegina
dc.subject Nanus
dc.subject Nummulites
dc.subject Nummulitidae
dc.subject Operculina (Foraminiferida)
dc.subject Sphaerogypsina
dc.title Sedimentary properties of the middle-upper eocene formations in çardak, burdur and incesu, SW Turkey
dc.title.alternative Çardak, Burdur ve İncesu havzalarında orta-üst eosen birimlerinin sedimanter özellikleri, GB Türkiye
dc.type Article
dc.relation.journal Turkish Journal of Earth Sciences
dc.contributor.authorID 0000-0002-1774-5012
dc.identifier.volume 21
dc.identifier.issue 3
dc.identifier.startpage 335
dc.identifier.endpage 373
dc.relation.publicationCategory Uluslararası Hakemli Dergi
dc.identifier.index Scopus
dc.identifier.index WOS
dc.identifier.index TRDizin

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