Palaeozoic deformation and magmatism in the northern area of the Anatolide block (Konya), witness of the Palaeotethys active margin

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dc.contributor.authorEren, Y
dc.contributor.authorKurt, H
dc.contributor.authorRosselet, F
dc.contributor.authorStampfli, GM
dc.date.accessioned2020-03-26T16:55:24Z
dc.date.available2020-03-26T16:55:24Z
dc.date.issued2004
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe study area. located north of Konva (Central Turkey), is composed of Silurian to Cretaceous metamorphosed rocks. The lower unit of the oldest formation (Silurian-Early Permian) is mostly made up of Silurian-Early Carboniferous metacarbonates. These rocks pass laterally and vertically to Devonian-Early Permian series having continental margin, shallow water and pelagic characteristics. They are intruded or juxtaposed to different kinds of metamagmatic rocks. which show MORB. continental arc and within plate characteristics. The Palaeozoic units are covered unconformably by Triassic-Cretaceous metasedimentary units. All these rocks are overthrusted by Mesozoic ophiolites. The Palaeozoic sequence can be seen as a northern Palaeotethys passive, then active margin. The northward subduction of the Palaeotethys ocean during the Carboniferous-Triassic times, induced the development of a magmatic arc and fore-arc sequence (Carboniferous-Permian). Before the Early Triassic (?Late Permian) time. the fore-arc sequence was uplifted above sea level and eroded. The Triassic sequences are regarded as marking the onset of back-arc opening and detachment of the Anatolian Konya block from the active Eurasian margin. Finally. a suture zone formed during the Carman between the Konya region and the Menderes-Tauride Cimmerian block due to the closing of Palaeotethvs. This geodynamic evolution can be correlated with the evolution of the Karaburun sequence in western Turkey.en_US
dc.identifier.doi10.1007/s00015-003-1131-8en_US
dc.identifier.endpage306en_US
dc.identifier.issn0012-9402en_US
dc.identifier.issue2en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage293en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s00015-003-1131-8
dc.identifier.urihttps://hdl.handle.net/20.500.12395/19155
dc.identifier.volume97en_US
dc.identifier.wosWOS:000225221800012en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherBIRKHAUSER VERLAG AGen_US
dc.relation.ispartofECLOGAE GEOLOGICAE HELVETIAEen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectMenderes-Tauride blocken_US
dc.subjectKonya regionen_US
dc.subjectCimmerianen_US
dc.subjectPalaeotethysen_US
dc.subjectmagmatic arcen_US
dc.subjectactive Eurasian marginen_US
dc.titlePalaeozoic deformation and magmatism in the northern area of the Anatolide block (Konya), witness of the Palaeotethys active marginen_US
dc.typeArticleen_US

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