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dc.contributor.advisorAkyazı, Mehmet
dc.contributor.authorTaşgit, Belgin
dc.date.accessioned2021-05-07T09:03:12Z
dc.date.available2021-05-07T09:03:12Z
dc.date.submitted2003
dc.date.issued2018-08-06
dc.identifier.urihttps://acikbilim.yok.gov.tr/handle/20.500.12812/604338
dc.description.abstract.
dc.description.abstractThe study area is located in the Paraouthoctonous Akseki tectonic segment wich issurrounded with Bey~ehir-Hoyran Nappe in the North, Yelekdag nappe in the south and issituated at the Tourid Belt. In this study, the stratigraphy and paleontology of the thickCarbonate Platforme ofLiassic-Lutetian age have been realized.The Jurassic-Cretaceous unit has Tithonic facies and contains Calpionellids in theregion. Tithonian-Berriasian boundary and stage separation of Tithonian-Berriasian havebeen done with these Calpionellids. But, they doesn't reach quantitatively abundant.Therefore, biostratigraphic studies haven't been realized to make mistake.en_US
dc.languageTurkish
dc.language.isotr
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAttribution 4.0 United Statestr_TR
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectJeoloji Mühendisliğitr_TR
dc.subjectGeological Engineeringen_US
dc.titleAkseki yöresinin stratigrafisi
dc.title.alternativeStratigraphy in Akseki region
dc.typemasterThesis
dc.date.updated2018-08-06
dc.contributor.departmentJeoloji Mühendisliği Ana Bilim Dalı
dc.identifier.yokid10039010
dc.publisher.instituteFen Bilimleri Enstitüsü
dc.publisher.universityCUMHURİYET ÜNİVERSİTESİ
dc.identifier.thesisid346882
dc.description.pages69
dc.publisher.disciplineDiğer


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