A Raman spectroscopic study of the phase transition in omphacite

Anna Katerinopoulou, Maurizio Musso, Georg Amthauer

10 Citationer (Scopus)

Abstract

Omphacites are very important in petrology because of their occurrence in rocks metamorphosed under high-pressure conditions. They have a wide thermobaric range of stability. Raman spectra of a natural, iron-bearing, ordered omphacite have been studied and compared with the experimentally disordered spectra. The order-disorder phase transition causes extra modes in the spectra. The ordering state affects the full width at half maximum (FWHM) of the main omphacite peak at 680 cm_1. Ordered omphacite shows a split peak around 1010 cm_1 caused by the slightly different orientation of tetrahedra in the monoclinic chain.
OriginalsprogEngelsk
TidsskriftVibrational Spectroscopy
Vol/bind48
Sider (fra-til)163-167
ISSN0924-2031
DOI
StatusUdgivet - 2008

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  • Det Natur- og Biovidenskabelige Fakultet

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