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dc.contributor.authorErol, Serap Colak
dc.contributor.authorOzkul, Mehmet
dc.contributor.authorAksoy, Ercan
dc.contributor.authorKele, Sandor
dc.contributor.authorGhaleb, Bassam
dc.date.accessioned16/12/21 12:07
dc.date.available16/12/21 12:07
dc.date.issued2015
dc.identifier.issn0985-3111
dc.identifier.urihttp://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/10545
dc.identifier.urihttps://doi.org/10.1080/09853111.2014.979530
dc.description.abstractThe Eastern Anatolian Fault System (EAFS) is a left-lateral strike-slip fault zone, 30km wide and 700km long, that is the second most important neotectonic structure of Turkey. In this study, relationship between travertine precipitation and tectonic acti
dc.description.sponsorshipScientific and Technological Research Council of Turkey - TUBITAKTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [110Y172]
dc.language.isoEnglish
dc.publisherTaylor & Francıs Ltd
dc.relation.ispartof17th Annual Meeting of Active Tectonic Study
dc.sourceGeodınamıca Acta
dc.titleTravertine occurrences along major strike-slip fault zones: structural, depositional and geochemical constraints from the Eastern Anatolian Fault System (EAFS), Turkey
dc.typeArticle; Proceedings Paper
dc.identifier.issue2-3
dc.identifier.startpage155
dc.identifier.endpage174
dc.identifier.doi10.1080/09853111.2014.979530
dc.identifier.wosWOS:000357090500005
dc.identifier.volume27


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