geochem2021-023_si_001.jpg (74.74 kB)

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.

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ORCID FOR SUBMITTING AUTHOR(s)

https://orcid.org/0000-0003-0311-4153
https://orcid.org/0000-0002-7942-1689
https://orcid.org/0000-0002-7103-422X

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Keywords

unresolved isobaric interferences dependent isotopic fractionation 57 56 fe versus δ samples yields pyrite plot linear line fe values analytical artefacts Geology

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