S. Carbonin et al., CATION DISTRIBUTION IN SOME NATURAL SPINELS FROM X-RAY-DIFFRACTION AND MOSSBAUER-SPECTROSCOPY, Mineralogical Magazine, 60(399), 1996, pp. 355-368
Three natural spinels of different places of occurrence and compositio
ns were investigated by means of microprobe chemical analysis, single
crystal X-ray diffraction and Mossbauer spectroscopy. All cation distr
ibutions between T and M sites were calculated from microprobe and XRD
experimental data, by means of a mathematical model with appropriate
assumptions. Fe2+ and Fe3+ assignments calculated in this way were com
pared with those observed in Mossbauer spectra. The satisfactory agree
ment found proves, at least in the samples studied, the reliability of
the model and the assumptions used. In the spinels examined, such res
ults show Fe2+ and Fe3+ virtually ordered in T and M sites respectivel
y. Mossbauer data also revealed Fe2+ in different tetrahedral sites du
e to the next-nearest neighbour effect, probably as a consequence of s
pinel genetic conditions.