Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/46184
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dc.contributor.authorDeniz, Kiymet-
dc.contributor.authorKadioglu, Yusuf Kagan-
dc.contributor.authorKoralay, Tamer-
dc.contributor.authorGüllü, Bahattin-
dc.date.accessioned2023-01-09T21:09:49Z-
dc.date.available2023-01-09T21:09:49Z-
dc.date.issued2021-
dc.identifier.issn0026-4563-
dc.identifier.urihttps://doi.org/10.19111/bulletinofmre.901035-
dc.identifier.urihttps://search.trdizin.gov.tr/yayin/detay/1116499-
dc.identifier.urihttps://hdl.handle.net/11499/46184-
dc.description.abstractFeldspar (alkali feldspar and plagioclases) and in recent years feldspathoid minerals are used as raw materials in the ceramic-glass industries. The igneous rocks such as granite, syenite and foid syenite which mainly contain these minerals have the potential to be raw materials. Some inclusions within the feldspatic minerals affect extremely negatively the desired values for raw material. In this study, the effective processes in the alteration of feldspatic minerals within the Ozvatan foid syenites, the effects of alteration minerals in the raw material were evaluated and the effects of the elements released by alteration on the environment were revealed. The foid syenites consist of nepheline, orthoclase, plagioclase, cancrinite, sodalite, amphibole, biotite, pyroxene, melanite with a rare amount of sphene, zircon, apatite and fluorite. The contents of the sericite and kaolinite, which are formed as a result of an alteration of these rocks, increase in direct proportion to alteration degree. As a result of the alteration index values, foid syenites samples show the low degreed decomposed property. According to the calculated mobility index (MI) from chemical analyses, there is a quantitative decrease in the major oxides such as SiO2, Al2O3, Na2O, K2O, CaO and Fe2O3 in the foid syenites. In accordance with the all data, Ozvatan foid syenites have been exposed both weathering and hydrothermal alteration and the effect of hydrothermal alteration are observed more frequently in the altered rock. While the excess of diaclase structures within the rock provides ease of operation, on the other hand, it accelerated the weathering and alteration processes.en_US
dc.language.isotren_US
dc.publisherMaden Tetkik Ve Arama Genel Mudurlugu-Mtaen_US
dc.relation.ispartofBulletin Of The Mineral Research And Explorationen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectFoid Syeniteen_US
dc.subjectAlterationen_US
dc.subjectGlass and Ceramic Raw Materialen_US
dc.subjectOzvatanen_US
dc.subjectCentral Anatoliaen_US
dc.subjectHydrothermal Alterationen_US
dc.subjectNormative Mineralsen_US
dc.subjectTrace-Elementsen_US
dc.subjectIgneous Rocksen_US
dc.subjectIndexesen_US
dc.subjectGeochemistryen_US
dc.subjectChemistryen_US
dc.subjectDepositsen_US
dc.subjectProvinceen_US
dc.subjectGranitesen_US
dc.titleThe distribution of elements in the alteration of feldspatic mineralsen_US
dc.typeArticleen_US
dc.identifier.volume166en_US
dc.identifier.startpage167en_US
dc.identifier.endpage188en_US
dc.identifier.doi10.19111/bulletinofmre.901035-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorscopusid57202922122-
dc.authorscopusid55621568600-
dc.authorscopusid16549984600-
dc.authorscopusid56528351100-
dc.authorwosidKORALAY, Tamer/V-8024-2017-
dc.identifier.scopus2-s2.0-85138755783en_US
dc.identifier.trdizinid1116499en_US
dc.identifier.wosWOS:000754380200010en_US
dc.identifier.scopusqualityQ3-
item.languageiso639-1tr-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.fulltextWith Fulltext-
item.openairetypeArticle-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
TR Dizin İndeksli Yayınlar Koleksiyonu / TR Dizin Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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