Oxidation during metasomatism in ultramafic xenoliths from the Wesselton kimberlite, South Africa: implications for the survival of diamond
Garnets in xenoliths from the Wesselton kimberlite show significant zoning in major and trace elements. The garnets were studied using room temperature Mössbauer spectroscopy with high spatial resolution, and show an increase in Fe3+/ΣFe from core to se
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|Source:||Contributions to Mineralogy and Petrology|
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