Geochemical characteristics of the Sebinkarahisar granitoids in the Eastern Pontides, northeast Turkey: Petrogenesis and tectonic implications
dc.authorid | Ilbeyli, Nurdane/0000-0002-0557-8771 | |
dc.contributor.author | Ilbeyli, Nurdane | |
dc.date.accessioned | 2024-09-18T21:06:37Z | |
dc.date.available | 2024-09-18T21:06:37Z | |
dc.date.issued | 2008 | |
dc.department | Hatay Mustafa Kemal Üniversitesi | en_US |
dc.description.abstract | A series of Cretaceous to Eocene granitoids are present in the Eastern Pontides of northeastern Turkey. The Asarcik (Saplica, Catakhan), Eskine, and Saydere (Sebinkarahisar-Giresun) are the least-studied, thus least-understood plutons in the orogen. Rock assemblages range from monzonite to granite. They contain mainly K-feldspar, plagioclase, quartz, hornblende, biotite, and Fe-Ti oxides. They are high-K, calc-alkaline, and I-type granites. Chondrite-normalized REE patterns are fractionated and have small negative Eu anomalies. They show enrichment in LILE and LREE relative to HFSE, displaying features of arc-related granitoids. Low molar Al2O3/(FeO+MgO+TiO2) in combination with variable molar (Na2O+K2O)/(FeO+MgO+TiO2) ratios indicate that the magmas were derived from mafic lower-crustal source rocks. The Eu and Sr anomalies and unfractionated HREE Suggest the presence of plagioclase and absence of garnet in the source. | en_US |
dc.identifier.doi | 10.2747/0020-6814.50.6.563 | |
dc.identifier.endpage | 582 | en_US |
dc.identifier.issn | 0020-6814 | |
dc.identifier.issn | 1938-2839 | |
dc.identifier.issue | 6 | en_US |
dc.identifier.scopus | 2-s2.0-47249161698 | en_US |
dc.identifier.scopusquality | Q1 | en_US |
dc.identifier.startpage | 563 | en_US |
dc.identifier.uri | https://doi.org/10.2747/0020-6814.50.6.563 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12483/13733 | |
dc.identifier.volume | 50 | en_US |
dc.identifier.wos | WOS:000256394300004 | en_US |
dc.identifier.wosquality | Q2 | en_US |
dc.indekslendigikaynak | Web of Science | en_US |
dc.indekslendigikaynak | Scopus | en_US |
dc.language.iso | en | en_US |
dc.publisher | Taylor & Francis Inc | en_US |
dc.relation.ispartof | International Geology Review | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject | Neotethyan Convergence | en_US |
dc.subject | Trace-Element | en_US |
dc.subject | Amphibolite | en_US |
dc.subject | Batholith | en_US |
dc.subject | Evolution | en_US |
dc.subject | Origin | en_US |
dc.subject | Rocks | en_US |
dc.subject | Area | en_US |
dc.subject | Rize | en_US |
dc.title | Geochemical characteristics of the Sebinkarahisar granitoids in the Eastern Pontides, northeast Turkey: Petrogenesis and tectonic implications | en_US |
dc.type | Article | en_US |
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