Geochemical features of the Menteşe Formation dolostones (Rhaetian) in the Karacahisar-Kasımlar area (Isparta-Turkey)

Basit Öğe Kaydı
dc.authorid0000-0002-1021-1560en_US
dc.contributor.authorDinç, Salih
dc.contributor.authorÖzkan, Ali Müjdat
dc.date.accessioned2021-11-29T08:29:52Z
dc.date.available2021-11-29T08:29:52Z
dc.date.issued2018-08en_US
dc.departmentBatman Üniversitesi Mühendislik - Mimarlık Fakültesi Jeoloji Mühendisliği Bölümüen_US
dc.description.abstractThe purpose of this study is to determine the geochemical characteristics of the Menteşe dolostones (Rhaetian) in the west Taurus Mountains, Turkey. The isotope characteristics of the Menteşe dolostones show a variation in the δ18O values of the dolomites between + 1.35 and − 2.72‰ (VPDB) and a variation in the δ13C values of the dolomites between + 1.6 and + 3.33‰ (VPDB). Most of the Menteşe dolostone samples have positive oxygen isotope values; others have weak negative isotope values, which indicate early diagenetic development. In addition, oxygen, carbon, and strontium isotopes and trace element analyses suggest that these dolostones were probably resulted from insignificant recrystallizaion process than chemically similar fluids. Furthermore, Mn/Sr values of the Menteşe dolostones indicate that there is no significant diagenetic alteration. The total REE contents of the Menteşe Formation dolostones display a strong positive correlation with Si, Al, Fe, K, Ti, Ba, Rb and negative correlation with Mg, hence REE content is associated with in the first degree titanium-bearing minerals (probably sphene, rutile, anatase), second degree phosphate (apatite), and barium and rubidium-bearing minerals (probably barite). Ce anomalies versus Nd concentrations of the Menteşe dolostone samples indicate that these dolostones are formed in an anoxic environment. In addition, the K/Rb ratios of the Menteşe dolostones are not exposed to any metamorphism and indicate some diagenetic alteration. Calculated temperature values using δ18O values of the Menteşe dolostones yield precipitation temperatures of 17 to 42 °C, and suggest burial depths of 67 to 900 m. Sources of magnesium for dolomitization of the Menteşe Formation carbonates were most likely fluids from seawater and/or diagenetic brines (slightly modified seawater). The Menteşe dolostones formed as early diagenetic (Rhaetian to Cenomanian) in shallow burial areas at lower temperatures than seawater and/or diagenetic brines (slightly modified seawater).en_US
dc.identifier.citationDinç, S., Özkan, A.M. (2018). Geochemical features of the Menteşe Formation dolostones (Rhaetian) in the Karacahisar-Kasımlar area (Isparta-Turkey). Arabian Journal of Geosciences, 11 (16). DOI:https://dx.doi.org/10.1007/s12517-018-3802-1en_US
dc.identifier.issn1866-7511
dc.identifier.issue16en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage449en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s12517-018-3802-1
dc.identifier.urihttps://hdl.handle.net/20.500.12402/4117
dc.identifier.volume11en_US
dc.identifier.wosqualityQ4en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringerLinken_US
dc.relation.isversionof10.1007/s12517-018-3802-1en_US
dc.relation.journalArabian Journal of Geosciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/restrictedAccessen_US
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/us/*
dc.subjectShallow Burialen_US
dc.subjectIsotopeen_US
dc.subjectSea Wateren_US
dc.subjectLow Temperatureen_US
dc.subjectWest Tauridesen_US
dc.titleGeochemical features of the Menteşe Formation dolostones (Rhaetian) in the Karacahisar-Kasımlar area (Isparta-Turkey)en_US
dc.title.alternativeKaracahisar-Kasımlar bölgesindeki (Isparta-Türkiye) Menteşe Formasyonu dolostonlarının (Resiyen) jeokimyasal özelliklerien_US
dc.typeArticleen_US

Dosyalar

Orijinal paket
Listeleniyor 1 - 1 / 1
Küçük Resim Yok
İsim:
Geochemical features of the Menteşe Formation dolostones (Rhaetian).pdf
Boyut:
9.8 MB
Biçim:
Adobe Portable Document Format
Açıklama:
Tam Metin / Full Text
İndir
Lisans paketi
Listeleniyor 1 - 1 / 1
Küçük Resim Yok
İsim:
license.txt
Boyut:
1.44 KB
Biçim:
Item-specific license agreed upon to submission
Açıklama:
İndir

Koleksiyon

Mühendislik-Mimarlık Fakültesi, Jeoloji Mühendisliği Bölümü, Makale Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu
WoS İndeksli Yayınlar Koleksiyonu