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• W2017237162 abstract "Abstract Titanomaghemite occurs in a relatively fresh doleritic intrusion in an area of Precambrian gneiss in Minas Gerais, Brazil. It hosts exsolution lamellae of ilmenite and contains more than 90% of the iron in the ferric form. It is more resistant to weathering than the ilmenite and is inherited virtually unaltered by the resulting soils. Titanomaghemite, extracted as grains from a weathered rind of the rock, has lattice parameter a 0 = 0.8348(3) nm and has a canted spin structure due to substitution of non-magnetic ions on tetrahedral and octahedral sites of the spinel structure. The average canting angle is 32 ± 3° and canting occurs predominantly on the octahedral iron sublattice. Its formula, based on microprobe analysis and Mössbauer spectroscopy may be expressed as: where [] and {} denote ions on tetrahedral and octahedral sites, respectively. The spontaneous magnetization of the mineral is 36(3) J/T/kg." @default.
• W2017237162 created "2016-06-24" @default.
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• W2017237162 date "1989-06-01" @default.
• W2017237162 modified "2023-09-26" @default.
• W2017237162 title "An occurrence of a fully-oxidized natural titanomaghemite in basalt" @default.
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• W2017237162 doi "https://doi.org/10.1180/minmag.1989.053.371.04" @default.
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