Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi-Basoren, Malatya), Turkey

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dc.authoridIlbeyli, Nurdane/0000-0002-0557-8771
dc.contributor.authorOzgenc, I.
dc.contributor.authorIlbeyli, N.
dc.date.accessioned2024-09-18T21:02:56Z
dc.date.available2024-09-18T21:02:56Z
dc.date.issued2009
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description.abstractLate Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basoren regions (Malatya). The Hasancelebi and Basoren intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basoren intrusive rocks mainly contain feldspathoidal syenites that are cut by feldspathoid-bearing dykes. The Hasancelebi intrusive rocks show comparable field, petrographic and geochemical characteristics with A-type rocks. All intrusive rocks show enrichment in LILE and LREE relative to HFSE. The Th/Yb versus Ta/Yb diagram indicates that all magmatic rocks formed from an enriched mantle source region(s). The parental magma for the Basoren rocks has a higher intraplate component than that from the Hasancelebi rocks which could be attributed to mantle source heterogeneity before collision in east-central Anatolia. Either delamination of the thermal boundary layer or slab-breakoff are likely mechanisms for the initiation of post-collisional magmatism in the Hasancelebi-Basoren areas.en_US
dc.description.sponsorshipTUBITAK [YDABAG 105 Y 076]en_US
dc.description.sponsorshipThis work is part of a research project supported by TUBITAK (YDABAG 105 Y 076). We thank Prof. Dr. Ahmet SASMAZ and also Ulku KARAKURT, Mehmet AKBULUT for their help during the fieldwork. We specially thank to Prof. Dr. Donna L. WHITNEY for improving English in the manuscript. Constructive reviews by Drs. Andy BEARD, Prelevic DEJAN, Jose Affonso BROD and Moacir J. B. MACAMBIRA are acknowledged. We also thank Prof. Dr. L. G. Gwalani for editorial handling.en_US
dc.identifier.doi10.1007/s00710-008-0027-0
dc.identifier.endpage85en_US
dc.identifier.issn0930-0708
dc.identifier.issn1438-1168
dc.identifier.issue1-2en_US
dc.identifier.scopus2-s2.0-59649085750en_US
dc.identifier.scopusqualityQ2en_US
dc.identifier.startpage71en_US
dc.identifier.urihttps://doi.org/10.1007/s00710-008-0027-0
dc.identifier.urihttps://hdl.handle.net/20.500.12483/13143
dc.identifier.volume95en_US
dc.identifier.wosWOS:000262830000004en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringer Wienen_US
dc.relation.ispartofMineralogy and Petrologyen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectA-Type Granitoidsen_US
dc.subjectCrystalline Complexen_US
dc.subjectCollisionen_US
dc.subjectOriginen_US
dc.subjectMantleen_US
dc.subjectMineralizationen_US
dc.subjectEvolutionen_US
dc.subjectCrustalen_US
dc.subjectRocksen_US
dc.subjectAreaen_US
dc.titleGeochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi-Basoren, Malatya), Turkeyen_US
dc.typeArticleen_US

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