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- W2019013664 abstract "The use of Rb/Ba and Rb/Sr ratios as guides to tin mineralization has only local interest, because each of the correlations log Rb/Ba-log Sn and log Rb/Sr-log Sn of granitic series has a different slope in every area. The ternary relation between Rb, Ba and Cs is useful to distinguish between Sn-bearing granitic rocks and non-mineralized granitic rocks. The Sn-bearing granitic rocks are late differentiates of anatectic melts (S-type), with primary albite and muscovite, and greisenized granites with metasomatic albite and muscovite. They have high Sn, Rb contents, Rb/Ba and Rb/Sr ratios, and low Ba and Sr contents. The Portuguese Sn-bearing muscovite granites, aplites, pegmatites and hypothermal quartz veins have muscovites richer in Sn than those of greisenized granites. F and Sn of muscovites from Portuguese Sn-bearing granitic rocks are positively correlated. Cassiterite crystallization seems to be independent of fH2Of inHF and favoured by a decrease in fO2." @default.
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- W2019013664 date "1984-03-01" @default.
- W2019013664 modified "2023-09-23" @default.
- W2019013664 title "Geochemistry of tin-bearing granitic rocks" @default.
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- W2019013664 doi "https://doi.org/10.1016/0009-2541(84)90052-4" @default.
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