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Triassic arc-derived detritus in the Triassic Karakaya accretionary complex was not derived from either the S Eurasian margin (Istanbul terrane) or the N Gondwana margin (Taurides)

dc.contributor.authorRobertson, Alastair H.F.
dc.contributor.authorUSTAÖMER, TIMUR
dc.contributor.authorGerdes, Axel
dc.contributor.authorZulauf, Gernold
dc.contributor.authorUstaömer, Petek Ayda
dc.date.accessioned2021-03-05T10:46:43Z
dc.date.available2021-03-05T10:46:43Z
dc.identifier.citationUSTAÖMER T., Ustaömer P. A. , Robertson A. H. , Gerdes A., Zulauf G., "Triassic arc-derived detritus in the Triassic Karakaya accretionary complex was not derived from either the S Eurasian margin (Istanbul terrane) or the N Gondwana margin (Taurides)", European Geoscience Union, Viyana, Avusturya, 27 Nisan - 02 Mayıs 2014, cilt.16, ss.10091
dc.identifier.othervv_1032021
dc.identifier.otherav_a4e30d3f-e085-42d8-b428-38144a131112
dc.identifier.urihttp://hdl.handle.net/20.500.12627/110287
dc.language.isoeng
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectYerbilimleri
dc.subjectTemel Bilimler (SCI)
dc.titleTriassic arc-derived detritus in the Triassic Karakaya accretionary complex was not derived from either the S Eurasian margin (Istanbul terrane) or the N Gondwana margin (Taurides)
dc.typeBildiri
dc.contributor.departmentYıldız Teknik Üniversitesi , ,
dc.identifier.volume16
dc.contributor.firstauthorID423835


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