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 Karadağ Stratovolcano in Central Anatolia, Turkey

dc.contributor.author	Çoban, H.
dc.contributor.author	Karsli, O.
dc.contributor.author	Caran, S.
dc.contributor.author	Yilmaz, K.
dc.date.accessioned	2021-12-16T10:12:04Z
dc.date.available	2021-12-16T10:12:04Z
dc.date.issued	2019
dc.identifier.issn	244937
dc.identifier.uri	https://doi.org/10.1016/j.lithos.2018.11.034
dc.identifier.uri	http://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/12970
dc.description.abstract	The Latest Cenozoic absarokite to shoshonite-banakite series (ASB) samples were discovered in the Karadağ 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	Türkiye Bilimsel ve Teknolojik Araştirma Kurumu, TÜBITAK: 107Y207
dc.language.iso	English
dc.publisher	Elsevier B.V.
dc.source	Lithos
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 Karadağ 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.scopus	2-s2.0-85058156273
dc.identifier.volume	324-325

Files in this item

Files	Size	Format	View
There are no files associated with this item.