Geological Society of London
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Formation of the high-grade Triple R uranium deposit revealed by Fe and S isotopes in pyrite

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posted on 2022-06-02, 11:34 authored by S. Mount, E. G. Potter, Z. Yang, M. Fayek, J. W. Powell, G. Chi, H. Rizo
Plot of δ57Fe versus δ56Fe values of samples yields a linear line with a slope of 1.46, consistent with mass-dependent isotopic fractionation and no analytical artefacts from unresolved isobaric interferences.