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A chemical examination of ilmenite sands, of New Zealand

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dc.contributor.author Wilks, Clyde Bannister
dc.date.accessioned 2011-12-13T21:29:34Z
dc.date.accessioned 2022-10-31T22:10:16Z
dc.date.available 2011-12-13T21:29:34Z
dc.date.available 2022-10-31T22:10:16Z
dc.date.copyright 1955
dc.date.issued 1955
dc.identifier.uri https://ir.wgtn.ac.nz/handle/123456789/27187
dc.description.abstract The 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.format pdf en_NZ
dc.language en_NZ
dc.language.iso en_NZ
dc.publisher Te Herenga Waka—Victoria University of Wellington en_NZ
dc.title A chemical examination of ilmenite sands, of New Zealand en_NZ
dc.type Text en_NZ
vuwschema.type.vuw Awarded Research Masters Thesis en_NZ
thesis.degree.discipline Science en_NZ
thesis.degree.grantor Te Herenga Waka—Victoria University of Wellington en_NZ
thesis.degree.level Masters en_NZ
thesis.degree.name Master of Science en_NZ


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