Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2357
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dc.contributor.authorallGoncuoglu, M. C.en
dc.date.accessioned2007-08-23T15:41:01Zen
dc.date.available2007-08-23T15:41:01Zen
dc.date.issued2004en
dc.identifier.urihttp://hdl.handle.net/2122/2357en
dc.description.abstractThe arkosic sandstones with olistostromes within the "Karakaya Complex" in NW Anatolia to the south of Geyve include a thin layer of green chert with radiolaria. Based on the composition of Albaillellids, the radiolarian assemblage corresponds to the Neoalbaillella ornithoformisassemblage, and its age is assigned to the Changxingian (Late Permian). This is the first finding of synsedimentary radiolarian cherts within the Karakaya units and the indication of latest Permian rifting of the Karakaya basin within the Midian carbonate platform and its pre-Permian basement in the Sakarya Composite Terrane.en
dc.language.isoEnglishen
dc.publisher.nameTUBITAKen
dc.relation.ispartofTurkish Journal of Earth Sciencesen
dc.relation.ispartofseries13en
dc.subjectChangxingian radiolariaen
dc.titleUpper Permian (Changxingian) Radiolarian Cherts within the Clastic Successions of the "Karakaya Complex" in NW Anatoliaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber201-213en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrologyen
dc.contributor.affiliationMETU Dept. Geol. Eng.en
dc.description.fulltextopenen
dc.contributor.authorGoncuoglu, M. C.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptMETU, Dept. of Geological Engineering, Ankara, Turkey-
crisitem.classification.parent04. Solid Earth-
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