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• W2174259034 abstract "The selective flux of sulfur during magma emplacement is proposed to explain some abnormal δ34S data from granitic and basaltic rocks. It is assumed that on the one hand a quasi-equilibrium isotope fractionation exists between sulfate and sulfide during magma cooling, and on the other hand a non-equilibrium fractionation occurs between the fluxed sulfur and the magmatic sulfur. The results show that at high fO2, 34S is preferably enriched in sulfate with decreasing temperature, without a corresponding depletion of sulfide in 34S. The δ34S value of solidified rocks is then significantly shifted in the positive direction due to the selective degassing or assimilation. Conversely, at low fO2, 34S is preferably depleted in sulfide as temperature declines, while a corresponding 34S-enrichment in sulfate does not occur. As a consequence, δ34S value of the rocks is driver in the negative direction." @default.
• W2174259034 created "2016-06-24" @default.
• W2174259034 creator A5038855167 @default.
• W2174259034 date "1990-01-01" @default.
• W2174259034 modified "2023-10-18" @default.
• W2174259034 title "The Selective Flux of Sulfur and Implications for Magmatic Sulfur Isotope Fractionation" @default.
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• W2174259034 doi "https://doi.org/10.1080/10256019008624335" @default.
• W2174259034 hasPublicationYear "1990" @default.
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