Unusually Y-rich monazite-(Ce) with 6–14 wt.% Y2O3 in a granulite from the Bohemian Massif: implications for high temperature monazite growth from the monazite-xenotime miscibility gap thermometry

Author: Krenn E.   Finger F.  

Publisher: Mineralogical Society

ISSN: 0026-461X

Source: Mineralogical Magazine, Vol.74, Iss.2, 2010-04, pp. : 217-225

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Abstract