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- W2321288081 abstract "The partitioning of Mg2+, Fe2+ and Mn2+ ions between spinel group minerals (spinel and magnetite series minerals) and 1 molal aqueous chloride solution was experimentally investigated at 600°C and 1 kb using standard cold-seal type pressure vessels. The experiments were carried out for the following six binary systems; spinel-hercynite, hercynite-galaxite, galaxite-spinel, magnesioferrite-magnetite, magnetite-jacobsite and jacobsite-magnesioferrite. Continuous solid solutions were formed in all of the systems. The cations are preferentially partitioned into the spinel series minerals in the order of Mg2+>Fe2+>Mn2+, and into the magnetite series minerals in the order of Fe2+>Mg2+>Mn2+. The cation partitioning between spinel and magnetite series minerals was derived from the above experimental results, which indicates that the formers prefer Mg2+ but the latters Fe2+ and Mn2+." @default.
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- W2321288081 date "1994-01-01" @default.
- W2321288081 modified "2023-10-16" @default.
- W2321288081 title "Experiments for the partitioning of Mg2+, Fe2+ and Mn2+ ions between spinel group minerals and aqueous chloride solution at 600.DEG.C. and 1 kb." @default.
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- W2321288081 doi "https://doi.org/10.2465/ganko.89.177" @default.
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