Chemical composition of monazite- and zircon-group minerals from the Dolní Bory pegmatites, Czech Republic ? Markers of the pegmatite evolution
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00083360" target="_blank" >RIV/00216224:14310/15:00083360 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Chemical composition of monazite- and zircon-group minerals from the Dolní Bory pegmatites, Czech Republic ? Markers of the pegmatite evolution
Original language description
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.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů