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- W2058710181 abstract "A mineral chemical investigation has been made on coexisting biotite, Caamphibole and iron oxides from the metamorphosed iron formation in Grängesberg, Sweden. The distribution of major and trace elements among these minerals is investigated. The distribution for most of the elements was found to be regular, indicating a close approach to chemical equilibrium between the coexisting phases. The mineral compositions are shown to be restricted by the pressure of oxygen which varies within the iron formation. Deviations in the distribution coefficients for Ti and Mn are found to be related to the content of tetrahedral Al in Ca-amphibole and Mn in Ca-amphibole respectively. Fractionation of the transition elements was found to be dependent on their respective crystal field stabilization in octahedral environments." @default.
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- W2058710181 date "1971-01-01" @default.
- W2058710181 modified "2023-09-27" @default.
- W2058710181 title "Distribution of major and minor elements in coexisting minerals from a metamorphosed iron formation" @default.
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- W2058710181 doi "https://doi.org/10.1016/0024-4937(71)90108-3" @default.
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