Sediment-derived melt-related metasomatized mantle wedge as a source of post-subduction Quaternary adakitic porphyries associated with absarokite-shoshonite from the Karadağ stratovolcano (Karaman, Central Anatolia, Turkey)

dc.contributor.author	Coban, H.
dc.contributor.author	Karsli, O.
dc.contributor.author	Caran, S.
dc.contributor.author	Yilmaz, K.
dc.date.accessioned	2021-12-16T10:11:49Z
dc.date.available	2021-12-16T10:11:49Z
dc.date.issued	2020
dc.identifier.issn	13679120
dc.identifier.uri	https://doi.org/10.1016/j.jseaes.2020.104380
dc.identifier.uri	http://dspace.beu.edu.tr:8080/xmlui/handle/20.500.12643/12763
dc.description.abstract	The Karadağ stratovolcano (KS), located at the southern end of the Cappadocian Volcanic Province in Central Anatolia, Turkey, is a key volcanic vent for understanding the spatiotemporal association between adakitic and mafic potassic (absarokitic-shoshoni
dc.description.sponsorship	Türkiye Bilimsel ve Teknolojik Araştirma Kurumu, TÜBITAK: 107Y207
dc.language.iso	English
dc.publisher	Elsevier Ltd
dc.source	Journal of Asian Earth Sciences
dc.title	Sediment-derived melt-related metasomatized mantle wedge as a source of post-subduction Quaternary adakitic porphyries associated with absarokite-shoshonite from the Karadağ stratovolcano (Karaman, Central Anatolia, Turkey)
dc.type	Article
dc.identifier.doi	10.1016/j.jseaes.2020.104380
dc.identifier.scopus	2-s2.0-85085121771
dc.identifier.volume	196

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