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dc.contributor.authorOzgen-Erdem, Nazire
dc.contributor.authorKoc-Tasgin, Calibe
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:37:03Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:37:03Z
dc.date.issued2019
dc.identifier.issn0016-7622
dc.identifier.issn0974-6889
dc.identifier.urihttps://dx.doi.org/10.1007/s12594-019-1249-y
dc.identifier.urihttps://hdl.handle.net/20.500.12418/5887
dc.descriptionWOS: 000471294100010en_US
dc.description.abstractIlerdian (early Eocene) carbonates in the northwestern Tosya region, northern Turkey, are characterized by porcellaneous larger benthic foraminifera; Glomalveolina, Alveolina, Orbitolites, Opertorbitolites and Cyclopertorbitolites are common in the southeastern Kastamonu region, in facies deposited on a low-gradient carbonate ramp. The inner ramp comprises of Miliolid-soritid wackestone, Soritid wackestone, Alveolinid-soritid wackestone-packstone, Alveolinid wackestone, Alveolinid-Nummulitid wackestone-packstone, algal wackestone, and Coralline algal pack-grainstone microfacies. The middle ramp deposits are composed of Alveolinid-nummulitid wackestone-packstone and Nummulitid wackestone-packstone microfacies. Overall, the succession reflects a long term deepening trend.en_US
dc.language.isoengen_US
dc.publisherSPRINGER INDIAen_US
dc.relation.isversionof10.1007/s12594-019-1249-yen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titleMicrofacies and Depositional Environment of the Ilerdian Carbonates in the North-Western Tosya (SE Kastamonu) Region, Northern Turkeyen_US
dc.typearticleen_US
dc.relation.journalJOURNAL OF THE GEOLOGICAL SOCIETY OF INDIAen_US
dc.contributor.department[Ozgen-Erdem, Nazire] Cumhuriyet Univ, Dept Geol Engn, Sivas, Turkey -- [Koc-Tasgin, Calibe] Firat Univ, Dept Geol Engn, Elazig, Turkeyen_US
dc.identifier.volume93en_US
dc.identifier.issue6en_US
dc.identifier.endpage712en_US
dc.identifier.startpage704en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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