Abstract:Chromian garnets occur within three podiform chromitite deposits in south-eastern N.S.W. Fourteen new analyses of these garnets are presented in this paper and these reveal that the garnets are either uvarovite or chromian grossular in composition. These analyses, along with analyses of uvarovite garnets from other world occurrences, suggest that there is no distinct relationship between the composition of uvarovite garnets and the geological setting in which they occur. Although the composition of the chromiu… Show more
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