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A chemical examination of ilmenite sands, of New Zealand

dc.contributor.authorWilks, Clyde Bannister
dc.date.accessioned2011-12-13T21:29:34Z
dc.date.accessioned2022-10-31T22:10:16Z
dc.date.available2011-12-13T21:29:34Z
dc.date.available2022-10-31T22:10:16Z
dc.date.copyright1955
dc.date.issued1955
dc.description.abstractThe black sands of New Zealand contain two main heavy detrital minerals, both of which are iron ores. They are titanomagnetic and ilmenite. The former has received close attention because of its possible utilization as the basis of an iron and steel industry, but it has been only in the last ten years that ilmenite has received close scrutiny. This has arisen from the realisation that our ilmenite-bearing sands are a vast store of raw material from which the desirable pigment titanium dioxide may be extracted, and even more important, the metal titanium. Titanium is a scarce metal today, and the demand is growing apace. Its unique physical properties make it a premium metal on the world's markets. Suggestions have been made that our ilmenite and titanomagnetite could be used for foundry work and steelmaking.en_NZ
dc.formatpdfen_NZ
dc.identifier.urihttps://ir.wgtn.ac.nz/handle/123456789/27187
dc.languageen_NZ
dc.language.isoen_NZ
dc.publisherTe Herenga Waka—Victoria University of Wellingtonen_NZ
dc.subjectSand
dc.subjectTitanium
dc.subjectNew Zealand sand
dc.titleA chemical examination of ilmenite sands, of New Zealanden_NZ
dc.typeTexten_NZ
thesis.degree.disciplineScienceen_NZ
thesis.degree.grantorTe Herenga Waka—Victoria University of Wellingtonen_NZ
thesis.degree.levelMastersen_NZ
thesis.degree.nameMaster of Scienceen_NZ
vuwschema.type.vuwAwarded Research Masters Thesisen_NZ

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