Peridotite hosted chromite, magnesite and olivine deposits of West Anatolia: A review

dc.contributor.authorZedef, Veysel
dc.date.accessioned2020-03-26T19:25:35Z
dc.date.available2020-03-26T19:25:35Z
dc.date.issued2016
dc.departmentSelçuk Üniversitesien_US
dc.descriptionInternational Conference on Advances in Natural and Applied Sciences (ICANAS) -- APR 21-23, 2016 -- Antalya, TURKEYen_US
dc.description.abstractTurkey has important chromite, magnesite and olivine deposits within peridotite host rocks. The peridotites (harzburgite, verlite, lherzolite and dunite) are mostly serpentinised as a result of metasomatic reaction of olivine and pyroxene minerals with percolating water. The serpentinites are generally an important part of ophiolitic complexes which displays a discontinuous belts all over the country. The chromite deposits are often related to cumulates and tectonites (as Alpine and/or podiform type deposits) and despite their small reserves, their grade can reach up to 58 %. In most deposits, a little enrichment efforts, the grade of chromite can easily be reached from 25 % to 40-45 %.en_US
dc.identifier.doi10.1063/1.4945943en_US
dc.identifier.isbn978-0-7354-1373-3
dc.identifier.issn0094-243Xen_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.urihttps://dx.doi.org/10.1063/1.4945943
dc.identifier.urihttps://hdl.handle.net/20.500.12395/33873
dc.identifier.volume1726en_US
dc.identifier.wosWOS:000376001000117en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherAMER INST PHYSICSen_US
dc.relation.ispartofINTERNATIONAL CONFERENCE ON ADVANCES IN NATURAL AND APPLIED SCIENCES: ICANAS 2016en_US
dc.relation.ispartofseriesAIP Conference Proceedings
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.titlePeridotite hosted chromite, magnesite and olivine deposits of West Anatolia: A reviewen_US
dc.typeConference Objecten_US

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