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dc.contributor.authorKarsli, Orhan
dc.contributor.authorCaran, Semsettin
dc.contributor.authorCoban, Hakan
dc.contributor.authorSengun, Firat
dc.contributor.authorTekkanat, Osman
dc.contributor.authorAndersen, Tom
dc.date.accessioned16/12/21 12:06
dc.date.available16/12/21 12:06
dc.date.issued2020
dc.identifier.issn0024-4937
dc.identifier.urihttp://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/9931
dc.identifier.urihttps://doi.org/10.1016/j.lithos.2020.105614
dc.description.abstractLate Cenozoic tectono-thermal events and associated magmatism in the Sakarya Zone (SZ) are still contested. Although documented in the western part of the SZ, thus far, no magmatic activity has been identified in the eastern part of the Oligocene SZ. Here
dc.description.sponsorshipSuleyman Demirel UniversitySuleyman Demirel University [SDUBAPKB 2205-YL-10]; Hefei University of Technology, China
dc.language.isoEnglish
dc.publisherElsevıer
dc.sourceLıthos
dc.titleMelting of the juvenile lower crust in a far-field response to roll-back of the southern Neotethyan oceanic lithosphere: the Oligocene adakitic dacites, NE Turkey
dc.typeArticle
dc.identifier.doi10.1016/j.lithos.2020.105614
dc.identifier.wosWOS:000558896300009
dc.identifier.volume370


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