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New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane

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dc.creator ÖKSÜM, Erdinç
dc.creator Hisarli, Z. Mumtaz
dc.creator Cinku, Mualla Cengiz
dc.creator Ustaomer, Timur
dc.creator Orbay, Naci
dc.date 2015-11-27T22:00:00Z
dc.date.accessioned 2020-10-06T09:48:13Z
dc.date.available 2020-10-06T09:48:13Z
dc.identifier 3ec09fe0-81c7-408f-813b-9b9237f5f4d7
dc.identifier 10.1016/j.tecto.2015.08.014
dc.identifier https://avesis.sdu.edu.tr/publication/details/3ec09fe0-81c7-408f-813b-9b9237f5f4d7/oai
dc.identifier.uri http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/58137
dc.description The Istanbul terrane, classically known as the "Paleozoic of Istanbul", is geologically one of the important continental components of NW Turkey. The terrane comprises an Early Ordovician to Early Carboniferous transgressive sedimentary sequence and appears as an exotic unit with respect to its present surroundings.
dc.language eng
dc.rights info:eu-repo/semantics/closedAccess
dc.title New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane
dc.type info:eu-repo/semantics/article


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