The geochronology and origin of mantle sources for late cenozoic intraplate volcanism in the frontal part of the Arabian plate in the Karacadag neovolcanic area of Turkey. Part 1. The results of isotope-geochronological studies

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dc.contributor.authorKeskin, M.
dc.contributor.authorChugaev, A. V.
dc.contributor.authorLebedev, V. A.
dc.contributor.authorSharkov, E. V.
dc.contributor.authorOyan, V.
dc.contributor.authorKavak, O.
dc.date.accessioned2024-04-24T17:11:54Z
dc.date.available2024-04-24T17:11:54Z
dc.date.issued2012
dc.departmentDicle Üniversitesien_US
dc.description.abstractThis paper considers results from isotope-geochronological (K-Ar) studies of the products of Neogene-Quaternary volcanism in the Karacadag area, which is situated within the northern frontal part of the Arabian plate. It was found that magmatic activity has been evolving at this location for at least the last 11-10 Myr and was distinctly discrete in character. Three stages of volcanism have been identified: (I) Early or Miocene, similar to 11-6.7 Ma; (II) Middle or Pliocene-Early Quaternary, 4-1 Ma; and (III) Late or Late Quaternary, 0.4-0.1 Ma. The most recent manifestations of magmatic activity in the region date back to about 100000 years ago. An analysis of the spatial distribution of volcanic centers of different ages in the Karacadag neovolcanic area shows that the magmatism of that region involved a lateral migration of activity from northwest to southeast along a major regional tectonic fault. The migration was caused by the movement of local tension zones where the lithosphere was thinner and deep-seated mantle magmas were ascending.en_US
dc.description.sponsorshipPresidium of the Russian Academy of Sciences; Russian Foundation for Basic Research [11-05-00012]; Scientific and Technological Research Council of Turkey [108Y222]en_US
dc.description.sponsorshipThis work was supported by Basic Research Program 4 of the Presidium of the Russian Academy of Sciences together with the Russian Foundation for Basic Research (no. 11-05-00012) and by the Scientific and Technological Research Council of Turkey (i.e., TUBITAK project no. 108Y222).en_US
dc.identifier.doi10.1134/S0742046312060036
dc.identifier.endpage360en_US
dc.identifier.issn0742-0463
dc.identifier.issn1819-7108
dc.identifier.issue6en_US
dc.identifier.scopus2-s2.0-84872020424
dc.identifier.scopusqualityQ3
dc.identifier.startpage352en_US
dc.identifier.urihttps://doi.org/10.1134/S0742046312060036
dc.identifier.urihttps://hdl.handle.net/11468/17768
dc.identifier.volume6en_US
dc.identifier.wosWOS:000313193500003
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoenen_US
dc.publisherPleiades Publishing Incen_US
dc.relation.ispartofJournal of Volcanology and Seismology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subject[No Keyword]en_US
dc.titleThe geochronology and origin of mantle sources for late cenozoic intraplate volcanism in the frontal part of the Arabian plate in the Karacadag neovolcanic area of Turkey. Part 1. The results of isotope-geochronological studiesen_US
dc.titleThe geochronology and origin of mantle sources for late cenozoic intraplate volcanism in the frontal part of the Arabian plate in the Karacadag neovolcanic area of Turkey. Part 1. The results of isotope-geochronological studies
dc.typeArticleen_US

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