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dc.contributor.authorYümün, Zeki Ünal
dc.contributor.authorKılıç, Ali Murat
dc.contributor.authorMartini, Rossana
dc.contributor.authorMetzger, Jacques
dc.contributor.authorTunç, Mahmut
dc.date.accessioned2019-10-23T06:49:58Z
dc.date.available2019-10-23T06:49:58Z
dc.date.issued2013en_US
dc.identifier.issn0016-6995
dc.identifier.issn1777-5728
dc.identifier.urihttps://doi.org/10.1016/j.geobios.2013.05.002
dc.identifier.urihttps://hdl.handle.net/20.500.12462/9148
dc.descriptionKılıç, Ali Murat (Balikesir Author)en_US
dc.description.abstractForaminifera have proven to be reliable biostratigraphic indicators. Accordingly, Triassic and Early Jurassic benthic Foraminifera allow us to define a biostratigraphic zonation within the carbonate platform of Kayseri (Yahyah), Goksun (Kahramanmara) and Sivas (Deliktas) regions in the Eastern Taurus (Ceviz, Aladag, Kaman and Felfan Mountains). Seven new stratigraphic sections are described in detail and the first precise inventory and illustration of the benthic foraminifer assemblages from the Triassic successions are presented over a large geographic area. The stratigraphic and palaeontological features of the Lower Mesozoic carbonate units of these mountains include several synchronous transgressive-regressive events that suggest continuity of the Lower Mesozoic environments over a large parautochthonous Taurus zone. Palaeogeographic considerations about the Eastern Taurus carbonates are given, evidencing three stages of development underwent by the studied area: 1) a stable continental margin from Lower Triassic to Lower Cretaceous; 2) a dismantling of the continental margin and first emplacement of ophiolites in the Upper Cretaceous; and 3) a deformation of the continental margin and emplacement of the Peridotite Nappe in the uppermost Cretaceous (Maastrichtian).en_US
dc.description.sponsorshipSwiss National Science Foundation (SNSF) - 200020-137661en_US
dc.language.isoengen_US
dc.publisherElsevier France-Editions Scientifiques Medicales Elsevieren_US
dc.relation.isversionof10.1016/j.geobios.2013.05.002en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectForaminiferaen_US
dc.subjectStratigraphyen_US
dc.subjectTriassicen_US
dc.subjectLower Jurassicen_US
dc.subjectTaurusen_US
dc.subjectTurkeyen_US
dc.titleLate Triassic and Lower Jurassic Foraminifera of the carbonate platform of the Beyaz Aladaǧ Group (Eastern Taurus, Turkey): New stratigraphic implicationsen_US
dc.typearticleen_US
dc.relation.journalGeobiosen_US
dc.contributor.departmentMühendislik - Mimarlık Fakültesien_US
dc.contributor.authorID0000-0002-0674-863Xen_US
dc.contributor.authorID0000-0003-4 679-1111en_US
dc.identifier.volume46en_US
dc.identifier.issue5en_US
dc.identifier.startpage447en_US
dc.identifier.endpage459en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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