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Titanium deposits in alkalic igneous rocks

January 1, 1975

Many types of alkalic rocks are enriched in Ti02 relative to the average for the crust. Silicate minerals in these rocks may have high Ti02 contents, but the oxides ilmenite, rutile, brookite, and perovskite are also characteristic primary phases. These tend to be higher in niobium than are the same minerals from other rock suites.

At Tapira, Brazil, titanium minerals in a carbonatite complex comprise tens of millions of tons contained Ti02. Anatase (as "leucoxene") is present in laterite lying over parent rocks containing perovskite, ilmenite, and rutile. In other discovered localities of alkalic rocks, production of titanium minerals is at best economically marginal.

Publication Year 1975
Title Titanium deposits in alkalic igneous rocks
DOI 10.3133/ofr7535
Authors Norman Herz
Publication Type Report
Publication Subtype USGS Numbered Series
Series Title Open-File Report
Series Number 75-35
Index ID ofr7535
Record Source USGS Publications Warehouse