About: Chemistry of xenotime-(Y) from beryl-columbite pegmatites of the Písek region (Czech Republic)     Goto   Sponge   NotDistinct   Permalink

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  • Xenotime-(Y) from the albite unit with abundant tourmaline of the beryl-columbite Písek granitic pegmatites have been studied with focus on monitoring of the mineral assemblages, successional position, chemical variability of xenotime, the input of U, Th and REE elements in the structure of the xenotime and to determine their substitution mechanisms.
  • Xenotime-(Y) from the albite unit with abundant tourmaline of the beryl-columbite Písek granitic pegmatites have been studied with focus on monitoring of the mineral assemblages, successional position, chemical variability of xenotime, the input of U, Th and REE elements in the structure of the xenotime and to determine their substitution mechanisms. (en)
Title
  • Chemistry of xenotime-(Y) from beryl-columbite pegmatites of the Písek region (Czech Republic)
  • Chemistry of xenotime-(Y) from beryl-columbite pegmatites of the Písek region (Czech Republic) (en)
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  • Chemistry of xenotime-(Y) from beryl-columbite pegmatites of the Písek region (Czech Republic)
  • Chemistry of xenotime-(Y) from beryl-columbite pegmatites of the Písek region (Czech Republic) (en)
skos:notation
  • RIV/00216224:14310/13:00074757!RIV15-MSM-14310___
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  • 65247
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  • RIV/00216224:14310/13:00074757
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  • xenotime-(Y); concentration of REE; uranium; thorium; substitution vector; granitic pegmatites; Písek (en)
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  • [A0F886C779AB]
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  • Losos, Zdeněk
  • Čopjaková, Renata
  • Švecová, Eva
  • Cicha, Jaroslav
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  • 14310
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