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Rationale
Quantifications of quadruple sulfur isotopic compositions (δ34S, Δ33S, and Δ36S) of sulfur‐bearing compounds in nature are valuable for providing new insights into the Earth's evolution such as the crust–mantle cycle, oxygenation of atmosphere and oceans, and the origin and evolution of early life. SF6‐based isotope ratio mass spectrometry is the most widely used method of quantification,...
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