dc.contributor.author | Yıldız, Ahmet | |
dc.contributor.author | Kibici, Yaşar | |
dc.contributor.author | Bağcı, Metin | |
dc.contributor.author | Dumlupunar, İbrahim | |
dc.contributor.author | Kocabaş, Cumhur | |
dc.contributor.author | Arıtan, Ali Ekrem | |
dc.date.accessioned | 2019-10-17T06:44:43Z | |
dc.date.available | 2019-10-17T06:44:43Z | |
dc.date.issued | 2015 | en_US |
dc.identifier.issn | 1866-7511 | |
dc.identifier.issn | 1866-7538 | |
dc.identifier.uri | https://doi.org/10.1007/s12517-015-1991-4 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12462/7360 | |
dc.description | Kocabaş, Cumhur (Balikesir Author) | en_US |
dc.description.abstract | Eocene volcanic rocks from the Central Sakarya Zone in the north of the A degrees zmir-Ankara suture zone (IASZ) are predominantly intermediate-acidic lava flows and pyroclastics that crop out with a W-E orientation. The volcanic rocks include Bozani double dagger lavas, agglomerates, A degrees AYdir lavas, and KapA +/- kaya tuffs. The Bozani double dagger lavas contain plagioclase, hornblende, clinopyroxene, and biotite, whereas the A degrees AYdir lavas consist of plagioclase, hornblende, biotite, and quartz. According to the total alkali-silica (TAS) diagram, the Bozani double dagger lavas are mainly composed of andesite and dacite, with one sample of trachyandesite, whereas the A degrees AYdir lavas mainly contain dacite and minor andesite. Bozani double dagger and A degrees AYdir lavas exhibit moderate- to high-K calc-alkaline character. Major oxide and trace element variations suggest the effects of fractional crystallization in the evolution of the volcanic rocks. N-type mid-ocean ridge basalt (MORB) normalized trace element patterns of the lavas exhibit enrichment in large ion lithophile elements (LILEs; K, Rb, Ba, Th) and depletion in high field strength elements (HFSEs; Zr, Ti, Y). In addition, the chondrite-normalized rare earth element (REE) plots of the rocks show moderately enriched and nearly concave-shaped patterns (La-N/Yb-N = 5.4-17.6 for the Bozani double dagger lavas and 6.5-13.1 for the A degrees AYdir lavas), suggesting clinopyroxene (Cpx) and hornblende dominated fractionation. Negative Eu anomalies in the acidic lavas reveal plagioclase fractionation. Some trace element ratios of the lavas demonstrate a subduction signature and crustal contamination in the generation of the parent magma(s). Multi-dimensional tectonic discrimination diagrams suggest that the studied volcanic rocks have developed in a collisional setting. | en_US |
dc.description.sponsorship | Scientific and Technical Research Council of Turkey (TUBITAK) | en_US |
dc.language.iso | eng | en_US |
dc.publisher | Springer Heidelberg | en_US |
dc.relation.isversionof | 10.1007/s12517-015-1991-4 | en_US |
dc.rights | info:eu-repo/semantics/embargoedAccess | en_US |
dc.subject | Post-collision | en_US |
dc.subject | Volcanism | en_US |
dc.subject | Calc-alkaline | en_US |
dc.subject | Sakarya Continent | en_US |
dc.subject | Turkey | en_US |
dc.title | Petrogenesis of the post-collisional Eocene volcanic rocks from the Central Sakarya Zone (Northwestern Anatolia, Turkey): Implications for source characteristics, magma evolution, and tectonic setting | en_US |
dc.type | article | en_US |
dc.relation.journal | Arabian Journal of Geosciences | en_US |
dc.contributor.department | Mühendislik-Mimarlık Fakültesi | en_US |
dc.contributor.authorID | 0000-0002-1056-2854 | en_US |
dc.contributor.authorID | 0000-0002-4967-3877 | en_US |
dc.identifier.volume | 8 | en_US |
dc.identifier.issue | 12 | en_US |
dc.identifier.startpage | 11239 | en_US |
dc.identifier.endpage | 11260 | en_US |
dc.relation.tubitak | info:eu-repo/grantAgreement/TUBITAK/104Y160 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |