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This page is a summary of: Stable H–C–O isotope and trace element geochemistry of the Cummins Range Carbonatite Complex, Kimberley region, Western Australia: implications for hydrothermal REE mineralization, carbonatite evolution and mantle source regions, Mineralium Deposita, September 2014, Springer Science + Business Media,
DOI: 10.1007/s00126-014-0552-1.
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