Natural Cr-spinels already characterized by X-ray single crystal diffraction and electron microprobe have been analyzed by Raman spectroscopy. The results we report show that there is a strong correlation between the Cr/(Cr+Al) ratio (Cr#) and the A1g mode for the studied spinels. A strong correlation of this mode with Mg/(Mg+Fe2+) (Mg#) can be seen only for spinels with Mg# higher than 0.60. Other modes can increase, decrease or disappear depending on the Cr#. Among the spinels with low Cr# it is possible to define their order/disorder degree. In fact, spinels with an inversion degree lower than 0.14 show an Eg mode at about 400-410 cm-1, while spinels with Cr# higher than 0.20 register the appearance of a peak in the region 150-200 cm-1, while other peaks are substituted by smooth curves. The results show that the use of Raman applied to spinel in provenance studies cannot yield a 100% confidence because of the uncertainties in the relation between Mg# and the different modes

Raman spectroscopy and the inversion degree of natural Cr-bearing spinels

LENAZ, DAVIDE;LUGHI, VANNI
2017

Abstract

Natural Cr-spinels already characterized by X-ray single crystal diffraction and electron microprobe have been analyzed by Raman spectroscopy. The results we report show that there is a strong correlation between the Cr/(Cr+Al) ratio (Cr#) and the A1g mode for the studied spinels. A strong correlation of this mode with Mg/(Mg+Fe2+) (Mg#) can be seen only for spinels with Mg# higher than 0.60. Other modes can increase, decrease or disappear depending on the Cr#. Among the spinels with low Cr# it is possible to define their order/disorder degree. In fact, spinels with an inversion degree lower than 0.14 show an Eg mode at about 400-410 cm-1, while spinels with Cr# higher than 0.20 register the appearance of a peak in the region 150-200 cm-1, while other peaks are substituted by smooth curves. The results show that the use of Raman applied to spinel in provenance studies cannot yield a 100% confidence because of the uncertainties in the relation between Mg# and the different modes
http://ammin.geoscienceworld.org/content/102/2/327
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11368/2901106
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