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dc.contributor.authorYeniyol, M.
dc.date.accessioned2021-03-03T10:59:38Z
dc.date.available2021-03-03T10:59:38Z
dc.date.issued2014
dc.identifier.citationYeniyol M., "Characterization of two forms of sepiolite and related Mg-rich clay minerals from Yenidogan (Sivrihisar, Turkey)", CLAY MINERALS, cilt.49, sa.1, ss.91-108, 2014
dc.identifier.issn0009-8558
dc.identifier.otherav_257d01dd-bc5c-4454-85c8-957c3a1cad8e
dc.identifier.othervv_1032021
dc.identifier.urihttp://hdl.handle.net/20.500.12627/30082
dc.identifier.urihttps://doi.org/10.1180/claymin.2014.049.1.08
dc.description.abstractAn Early Pliocene sedimentary succession in the Yenidogan area, Sivrihisar, Turkey, consists of sepiolite, stevensite, kerolite, dolomite and magnesite. The geology, mineralogy and geochemistry of the succession was examined by extensive field work along several trenches and a representative measured section, followed by X-ray diffraction (XRD), Fourier transform infrared spectroscopy (FTIR), scanning electron microscopy (SEM), thermal, and chemical analyses.
dc.language.isoeng
dc.subjectFizikokimya
dc.subjectTemel Bilimler
dc.subjectMühendislik ve Teknoloji
dc.subjectMİNERALOJİ
dc.subjectJeoloji Mühendisliği
dc.subjectJEOLOJİ
dc.subjectYerbilimleri
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.subjectTemel Bilimler (SCI)
dc.subjectKimya
dc.subjectKİMYA, FİZİKSEL
dc.titleCharacterization of two forms of sepiolite and related Mg-rich clay minerals from Yenidogan (Sivrihisar, Turkey)
dc.typeMakale
dc.relation.journalCLAY MINERALS
dc.contributor.department, ,
dc.identifier.volume49
dc.identifier.issue1
dc.identifier.startpage91
dc.identifier.endpage108
dc.contributor.firstauthorID213546


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