作者: R. Zboril , M. Mashlan , L. Machala , J. Walla , K. Barcova
DOI: 10.1007/978-1-4020-2852-6_61
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摘要: The natural garnets from almandine (Fe3Al2Si3O12)—pyrope (Mg3Al2Si3O12) series with the iron to magnesium atomic ratio ranging 0.2 1 were characterised and their thermal behaviour at 1200°C studied by 57Fe Mossbauer spectroscopy, X-ray powder diffraction, fluorescence, DTA, TG electron microprobe analysis. pyrope-type samples a dominant content position 24c in cubic garnet structure undergo oxidative decomposition resulting formation of paramagnetic spinel Mg(A1,Fe)204 low content, enstatite (Mg,Fe)SiO3 anorthite CaAl2Si2O8 as host compound for calcium. Contrary pyropes, iron-rich exhibit complete oxidation conforming magnetically ordered nanocrystalline γ-Fe2O3 or Mg(Fe,AI)2O4 spinels depending on initial chemical composition garnets. In reaction products garnets, cordierite (Mg2A14Si5O18) identified non-ferrous phases.