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Economic Geology; June 1959; v. 54; no. 4; p. 698-719
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Some mineralogical relationships in the system Fe 2 O 3 -Fe 3 O 4 and the composition of titanomaghemite

E. Z. Basta

Many maghemites, such as those of the Bushveld complex (Africa), are found to contain appreciable amounts of TiO 2 in their gamma -Fe 2 O 3 spinel structure. Such titanomaghemites are considered to be formed by oxidation of titanomagnetite, and the appreciable variation in their content of FeO and in the ratio FeO:TiO 2 can be explained on the basis of differences in composition of the original titanomagnetite and the degree of its oxidation.

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 Clays and Clay MineralsHome page
M. T. de Oliveira, M. T. G. de Oliveira, M. L. L. Formoso, M. I. da Costa Jr, and A. Meunier
THE TITANOMAGNETITE TO TITANOMAGHEMITE CONVERSION IN A WEATHERED BASALT PROFILE FROM SOUTHERN PARANA BASIN, BRAZIL
Clays and Clay Minerals, August 1, 2002; 50(4): 478 - 493.
[Abstract] [Full Text] [PDF]


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