What processes control the genesis of absarokite to shoshonite-banakite series in an intracontinental setting, as revealed by geochemical and Sr-Nd-Pb isotope data of Karadak Stratovolcano in Central Anatolia, Turkey

dc.contributor.author	Coban, Hakan
dc.contributor.author	Karsli, Orhan
dc.contributor.author	Caran, Semsettin
dc.contributor.author	Yilmaz, Kamil
dc.date.accessioned	2021-12-16T09:07:06Z
dc.date.available	2021-12-16T09:07:06Z
dc.date.issued	2019
dc.identifier.issn	0024-4937
dc.identifier.uri	https://doi.org/10.1016/j.lithos.2018.11.034
dc.identifier.uri	http://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/10193
dc.description.abstract	The Latest Cenozoic absarokite to shoshonite-banakite series (ASB) samples were discovered in the Karadag stratovolcano (KS) which erupted in the Karaman basin in Central Anatolia, Turkey; and has a spatially close association with major strike-slip fault
dc.description.sponsorship	Scientific and Technological Research Council of Turkey (TUBITAK)Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [107Y207]
dc.language.iso	English
dc.publisher	Elsevıer
dc.source	Lıthos
dc.title	What processes control the genesis of absarokite to shoshonite-banakite series in an intracontinental setting, as revealed by geochemical and Sr-Nd-Pb isotope data of Karadak Stratovolcano in Central Anatolia, Turkey
dc.type	Article
dc.identifier.startpage	609
dc.identifier.endpage	625
dc.identifier.doi	10.1016/j.lithos.2018.11.034
dc.identifier.wos	WOS:000457819800040
dc.identifier.volume	324

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