Phase investigation of an iron meteorite from Akyumak

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dc.contributor.authorAksoy, I
dc.contributor.authorCeylan, M
dc.contributor.authorKayali, N
dc.date.accessioned2026-08-12T17:40:19Z
dc.date.issued1996
dc.departmentFırat Üniversitesi
dc.description.abstractThe phase of an iron meteorite which fell near Akylumak, East Anatolia, in 1981 have been investigated by optical and X-ray diffraction. Diffraction peaks of kamacite, teanite, plessite and cementite phases were separated and indexed by the related unit cell parameters of the phases. From the analysis of DSC and DTA curves, some phase transformation are known to have occurred during different heating regimes.
dc.identifier.doi10.1016/0924-0136(95)02080-2
dc.identifier.endpage224
dc.identifier.issn0924-0136
dc.identifier.issue3.Nis
dc.identifier.scopus2-s2.0-0030079670
dc.identifier.scopusqualityQ1
dc.identifier.startpage221
dc.identifier.urihttps://doi.org/10.1016/0924-0136(95)02080-2
dc.identifier.urihttps://hdl.handle.net/11508/59231
dc.identifier.volume57
dc.identifier.wosWOS:A1996UQ66300002
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherElsevier Science Sa Lausanne
dc.relation.ispartofJournal of Materials Processing Technology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20260511
dc.titlePhase investigation of an iron meteorite from Akyumak
dc.typeArticle

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