Neogene volcanism in Elazig-Tunceli area (eastern Anatolia): geochronological and petrological constraints

Autor: Agostini S.[1], Savascin M.[2], Di Giuseppe P.[1, Di Stefano F.[4], Karaoglu O.[5], Lustrino M.[4, Manetti P.[7, Ersoy Y.[8], Kürüm S.[9], Önal A.[2]

Publikováno v: Italian Journal of Geosciences (Online) 138 (2019): 435–455.
info:cnr-pdr/source/autori:Agostini S.[1], Savascin M.[2], Di Giuseppe P.[1,3], Di Stefano F.[4], Karaoglu O.[5], Lustrino M.[4,6], Manetti P.[7,1], Ersoy Y.[8], Kürüm S.[9], Önal A.[2]/titolo:Neogene volcanism in Elazig-Tunceli area (eastern Anatolia): geochronological and petrological constraints/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2019/pagina_da:435/pagina_a:455/intervallo_pagine:435–455/volume:138

The Elaz?? and Tunceli provinces in eastern Anatolia host a complex succession of Miocene-Pleistocene effusive and explosive volcanic rocks, divided into four distinct volcanic phases. The most abundant and widespread products are the calcalkaline Ma

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http://www.cnr.it/prodotto/i/407686