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- W2091628246 abstract "F and Cl values are given for an albite granite plug which has crystallised from a peralkaline granite in northern Saudi Arabia and also for siliceous veins derived from the same peralkaline granite. The F contents (in ppm) are as follows: 425–1980 for the peralkaline granite (four samples). 12,190–14,675 for the albite granite (two samples) and 520–667 for the siliceous veins (two samples). The Cl contents are respectively 62–394, 45–205 and 223–510. Figures show the halogen and trace-element contents and REE patterns relative to chondrites for the same three rock types. The results indicate that F concentrates in the residual liquid of a peralkaline magma, whereas Cl concentrates in the coexisting volatile phase. Fluoride complexes may contribute to element mobility in peralkaline magma, but the presence of alkalis may be equally important in the formation of complexes. Carbonate complexing is the most plausible cause of element mobility in the veins." @default.
- W2091628246 created "2016-06-24" @default.
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- W2091628246 date "1980-01-01" @default.
- W2091628246 modified "2023-09-26" @default.
- W2091628246 title "The role of fluorine and chlorine in the petrogenesis of a peralkaline complex from Saudi Arabia" @default.
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- W2091628246 doi "https://doi.org/10.1016/0009-2541(80)90092-3" @default.
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