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6. The chemical conditions of the late Archean Hamersley basin inferred from whole rock and pyrite geochemistry with Δ33S and δ34S isotope analyses. (15th January 2015)

7. The formation mechanisms of sedimentary pyrite nodules determined by trace element and sulfur isotope microanalysis. (15th August 2019)

8. Whole rock and discrete pyrite geochemistry as complementary tracers of ancient ocean chemistry: An example from the Neoproterozoic Doushantuo Formation, China. (1st November 2017)