Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.13091/4254
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dc.contributor.authorKinaci, Eyyüp Hikmet-
dc.contributor.authorÖztürk, Alican-
dc.date.accessioned2023-05-31T20:19:34Z-
dc.date.available2023-05-31T20:19:34Z-
dc.date.issued2023-
dc.identifier.issn2296-6463-
dc.identifier.urihttps://doi.org/10.3389/feart.2023.1145674-
dc.identifier.urihttps://hdl.handle.net/20.500.13091/4254-
dc.description.abstractDiaspore, is related to bauxite in terms of its formation mechanism. Diaspore is one of the gemstone quality stones used in jewelry and jewelry making. It is possible to come across gemstones in various regions of the world. In our country, there are gemstone deposits in all regions. In these deposits, diaspore crystals are considered very valuable. Within the scope of this study, it was aimed to determine the gemological features of the diaspore formations in Sodra (Milas-Mugla) and its surroundings, as well as to determine other minerals and their formation conditions. Main oxide, trace, and rare earth element analyses were performed on seven collected samples. The classification was made using the Al2O3-SiO2-Fe2O3 triangular variation and it was determined that bauxite samples were in the ferric bauxite and bauxite areas. SEM imaging and EDS analyzes were performed on the samples and according to this result, it was determined that the samples mainly contained O, Al, and Si. The data obtained as a result of Raman Spectroscopy were matched with the device's own data library and it was determined that the samples taken from the Sodra region were diaspore. In addition, according to the results of the FTIR analysis performed on the faceted sample taken from the Sodra region, it was seen that the samples were compatible with the reference standards and it was scientifically proven to be a diaspore crystal with gemstone quality. During the field studies carried out in the study area, diaspore crystals were encountered in the Milas-Sodra region, together with chloritoid and muscovite, within the metabauxite formations and in the altered zones close to the metabauxite limestone contact. Rock were classified as muscovitequartzschist, quartzschist with grano-lepidoblastic texture, micaquartzschist with lepidoblastic texture, phyllite with lepidoblastic texture, and chlorite-epidote fels with nematoblastic texture as a result of petrographic analyzes performed on the country rock samples. It is predicted that these gemstone-quality diaspore crystals can be evaluated economically.en_US
dc.description.sponsorshipKonya Technical University Scientific Research Project Coordinator [201107007]en_US
dc.description.sponsorshipThis study was supported by Konya Technical University Scientific Research Project Coordinator (BAP Project No: 201107007).en_US
dc.language.isoenen_US
dc.publisherFrontiers Media Saen_US
dc.relation.ispartofFrontiers In Earth Scienceen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectgemologyen_US
dc.subjectmetabauxiteen_US
dc.subjectRaman spectroscopyen_US
dc.subjectSodraen_US
dc.subjectdiaspore (AlOOH)en_US
dc.subjectNorthern Guizhou Provinceen_US
dc.subjectBauxite Depositsen_US
dc.subjectGeochemical Investigationsen_US
dc.subjectElement Geochemistryen_US
dc.subjectIndia Implicationsen_US
dc.subjectMenderes Massifen_US
dc.subjectWestern Turkeyen_US
dc.subjectBlack Shalesen_US
dc.subjectMineralogyen_US
dc.subjectEvolutionen_US
dc.titleGemological features of diaspore in sodra-Milas (mugla) regionen_US
dc.typeArticleen_US
dc.identifier.doi10.3389/feart.2023.1145674-
dc.identifier.scopus2-s2.0-85152572118en_US
dc.departmentKTÜNen_US
dc.identifier.volume11en_US
dc.identifier.wosWOS:000967366300001en_US
dc.institutionauthor-
dc.relation.publicationcategoryMakale - Uluslararasi Hakemli Dergi - Kurum Ögretim Elemanien_US
dc.authorscopusid58184408900-
dc.authorscopusid7103003182-
dc.identifier.scopusqualityQ1-
item.grantfulltextopen-
item.fulltextWith Fulltext-
item.languageiso639-1en-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.openairetypeArticle-
crisitem.author.dept02.07. Department of Geological Engineering-
Appears in Collections:Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collections
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collections
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