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

dc.contributor.authorOrbay, Naci
dc.contributor.authorHisarli, Z. Mumtaz
dc.contributor.authorÖKSÜM, Erdinç
dc.contributor.authorCinku, Mualla Cengiz
dc.contributor.authorUstaomer, Timur
dc.date.accessioned2021-03-03T15:23:41Z
dc.date.available2021-03-03T15:23:41Z
dc.identifier.citationÖKSÜM E., Hisarli Z. M. , Cinku M. C. , Ustaomer T., Orbay N., "New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane", TECTONOPHYSICS, cilt.664, ss.14-30, 2015
dc.identifier.issn0040-1951
dc.identifier.otherav_3ec09fe0-81c7-408f-813b-9b9237f5f4d7
dc.identifier.othervv_1032021
dc.identifier.urihttp://hdl.handle.net/20.500.12627/46028
dc.identifier.urihttps://doi.org/10.1016/j.tecto.2015.08.014
dc.description.abstractThe 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.isoeng
dc.subjectYerbilimleri
dc.subjectMühendislik ve Teknoloji
dc.subjectJEOKİMYA VE JEOFİZİK
dc.subjectJeofizik Mühendisliği
dc.subjectTemel Bilimler (SCI)
dc.titleNew paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane
dc.typeMakale
dc.relation.journalTECTONOPHYSICS
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume664
dc.identifier.startpage14
dc.identifier.endpage30
dc.contributor.firstauthorID225914


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