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- W3080826097 abstract "The Salmi batholith’s successive felsic rocks differentiates are represented by a series: biotite-amphibole granite-rapakivi, biotite granite, highly differentiated granites (Li-siderophyllite granite and zinnwaldite Li-F granite). In this series of rocks a gradual increase in content of Ta and Nb and a decrease in the Nb/Ta ratio is seen. A regular change in the separation factors of Ta and Nb between mica and the total composition of the rock is observed as well. When comparing Li-siderophyllite granites and Li-F granites, the latter have a sharp decrease in the separation coefficients Kr Ta, Nb . This decrease is due to the fall in content of these metals in Li-F granites zinnwaldite and associated with the appearance of columbite in these rocks. The study of rock samples from the Salmi batholith suggests that the change of the Ta and Nb content in the mica of deeply differentiated granites and the corresponding decrease in the K r value of these metals may be a diagnostic indication of the presence of columbite mineralization in the rock." @default.
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- W3080826097 date "2019-06-28" @default.
- W3080826097 modified "2023-09-23" @default.
- W3080826097 title "Mica composition of Salmi batholith granites as an indicator of forming Nb-Ta mineralization" @default.
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- W3080826097 doi "https://doi.org/10.33623/0579-9406-2019-3-69-77" @default.
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