The relationship between collision-related calcalkaline, and within-plate alkaline volcanism in the Karacadag Area (Konya-Turkiye, Central Anatolia)

Basit Öğe Kaydı
dc.contributor.authorKurt, Hueseyin
dc.contributor.authorAsan, Kuersad
dc.contributor.authorRuffet, Gilles
dc.date.accessioned2020-03-26T17:28:14Z
dc.date.available2020-03-26T17:28:14Z
dc.date.issued2008
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe Karacadag (Kulu-Konya) area is one of the main volcanic provinces in Central Anatolia. The Karacadag volcanites are composed of large volumes of andesitic-dacitic lavas associated with pyroclastics and small volumes of alkali basalt, trachybasalt and trachyandesite lavas. Two groups of volcanic rocks can be distinguished: (1) calcalkaline rocks including andesites and dacites, and (2) alkaline rocks including basalts, trachybasalts and trachyandesites. Ar-40/Ar-39 ages show that the Karacadag volcanites were erupted during Early Miocene (ca. 18-19 Ma) and suggest that alkaline volcanites succeed shortly afterwards calcalkahne volcanites. Major oxides and trace elements plotted versus SiO2 Suggest fractionation of hornblende, Fe-Ti oxide and apatite for calcalkaline volcanic rocks and olivine, clinopyroxene and Fe-Ti oxide for alkaline volcanic rocks in the magmatic evolution. The incompatible trace element patterns of the calcalkaline volcanites show enrichment of LILEs (Sr, K, Rb, Ba and Th) and negative HFSEs (Nb, Ta) anomalies suggesting an enriched lithospheric source by a subduction-related process. On the other hand, alkaline volcanites show enrichment of both LILEs and HFSEs suggesting an enriched lithospheric source by small volume melts from the asthenosphere. The rocks also have moderately fractionated REE patterns with (La/LU)(N) ratios of 7-24 for calcalkaline and 6-17 for alkaline volcanites. Moreover, the volcanites have relatively low Sr-87/Sr-86(t) ratios for t = 18 Ma between 0.703782 and 0.705129, and high epsilon N-d(t) values between + 2.25 and + 4.49. Generally, the Sr-Nd isotopic compositions of the rocks range from the mantle array to bulk earth. All of these observations and findings suggest that the calcalkaline volcanites were formed in a subduction modified orogenic setting, and the alkaline volcanites in a within-plate setting. (C) 2006 Elsevier GmbH. All rights reserved.en_US
dc.description.sponsorshipSelcuk University Coordination of Scientific ResearchSelcuk University [05401043, 2003/186]en_US
dc.description.sponsorshipThis study was financially supported by a project numbers 05401043 and 2003/186 from the Selcuk University Coordination of Scientific Research Project (S.U. BAP) in Turkiye. The authors gratefully thank to the Selcuk University for its supports. Also, the authors thank to Lang Shi for microprobe analyses (McGill University, Canada), Dean Toye, Clarence Leong and Jacky Wang for ICP-MS and ICP-ES analyses (Acme Laboratories, Canada) and Jean-Jacques Peucat for Sr-Nd isotope analyses (CNRS-Universite de Rennes, France). Finally, the authors thank to Professor Dr. Martin Okrusch (Wurzburg University) for reviewing the manuscript.en_US
dc.identifier.doi10.1016/j.chemer.2006.05.003en_US
dc.identifier.endpage176en_US
dc.identifier.issn0009-2819en_US
dc.identifier.issn1611-5864en_US
dc.identifier.issue2en_US
dc.identifier.scopusqualityQ2en_US
dc.identifier.startpage155en_US
dc.identifier.urihttps://dx.doi.org/10.1016/j.chemer.2006.05.003
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22741
dc.identifier.volume68en_US
dc.identifier.wosWOS:000258809600003en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherELSEVIER GMBH, URBAN & FISCHER VERLAGen_US
dc.relation.ispartofCHEMIE DER ERDE-GEOCHEMISTRYen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectCentral Anatoliaen_US
dc.subjectKaracadag volcanitesen_US
dc.subjectalkalineen_US
dc.subjectAr-40/Ar-39 datingen_US
dc.subjectwithin-plateen_US
dc.titleThe relationship between collision-related calcalkaline, and within-plate alkaline volcanism in the Karacadag Area (Konya-Turkiye, Central Anatolia)en_US
dc.typeArticleen_US

Dosyalar

Koleksiyon

WoS İndeksli Yayınlar Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu