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Chemical composition of monazite- and zircon-group minerals from the Dolní Bory pegmatites, Czech Republic – Markers of the pegmatite evolution
Název česky | Chemické složení minerálů skupiny monazitu a zirkonu z pegmatitů v Dolních Borech – Ukazatel evoluce pegmatitů |
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Autoři | |
Rok publikování | 2015 |
Druh | Další prezentace na konferencích |
Fakulta / Pracoviště MU | |
Citace | |
Popis | Minerals of the monazite- and zircon-group from several pegmatite dykes near Dolní Bory were studied by EMPA. The results show significant fractionation of Sc and U, but no fractionation of Th in studied minerals during crystallization of the pegmatite dykes. Deep negative europium anomaly was present already in the border zone and is therefore inherited feature of the pegmatitic melt. On the other hand, M-type tetrad effect developed in-situ after dyke emplacement. |