Melting 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.contributor.author	Karsli, Orhan
dc.contributor.author	Caran, Semsettin
dc.contributor.author	Coban, Hakan
dc.contributor.author	Sengun, Firat
dc.contributor.author	Tekkanat, Osman
dc.contributor.author	Andersen, Tom
dc.date.accessioned	16/12/21 12:06
dc.date.available	16/12/21 12:06
dc.date.issued	2020
dc.identifier.issn	0024-4937
dc.identifier.uri	http://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/9931
dc.identifier.uri	https://doi.org/10.1016/j.lithos.2020.105614
dc.description.abstract	Late 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.sponsorship	Suleyman Demirel UniversitySuleyman Demirel University [SDUBAPKB 2205-YL-10]; Hefei University of Technology, China
dc.language.iso	English
dc.publisher	Elsevıer
dc.source	Lıthos
dc.title	Melting 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.type	Article
dc.identifier.doi	10.1016/j.lithos.2020.105614
dc.identifier.wos	WOS:000558896300009
dc.identifier.volume	370

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