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dc.contributor.authorAkyazi, M
dc.contributor.authorOzgen-Erdem, N
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T10:23:43Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T10:23:43Z
dc.date.issued2003
dc.identifier.issn0377-9211
dc.identifier.urihttps://hdl.handle.net/20.500.12418/11424
dc.descriptionWOS: 000184630400002en_US
dc.description.abstractThe Odemis Formation crops out around Odemis village to the northwest of the town of Ilgaz (Cankiri, Turkey). The Formation was deposited in neritic environments, and it consists of conglomerate, nodular limestone, sandstone, sandy limestone, and claystone, interbedded with volcanics. The sandy limestones contain the benthic foraminifera Orbitoides aff. medius (d'Archiac), O. aff. apiculatus Schlumberger, Sirelina orduensis Meric & Inan, Omphalocyclus macroporus (Lamarck), Sirtina orbitoidiformis Bronnimann & Wirtz, Praestorrsella roestae (Visser), Laffitteina bibensis Marie, Laffitteina boluensis Dizer, Laffitteina aff. marsicana Farinacci, Smoutina aff. cruysi Drooger, Siderolites calcitrapoides Lamarck, and Selimina spinalis Inan. Praestorrsella roestae (Visser) was abundant. This foraminiferal assemblage indicates an upper Maastrichtian age.en_US
dc.language.isoengen_US
dc.publisherKING FAHD UNIV PETROLEUM MINERALSen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titlePaleontology and stratigraphy of upper cretaceous sediments in the Ilgaz region (Cankiri, Turkey)en_US
dc.typearticleen_US
dc.relation.journalARABIAN JOURNAL FOR SCIENCE AND ENGINEERINGen_US
dc.contributor.departmentCumhuriyet Univ, Dept Geol Engn, TR-58140 Sivas, Turkeyen_US
dc.identifier.volume28en_US
dc.identifier.issue1Aen_US
dc.identifier.endpage34en_US
dc.identifier.startpage25en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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