| Reference Type | Journal (article/letter/editorial) |
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| Title | 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 |
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| Journal | Mineralogical Magazine |
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| Authors | Krenn, E. | Author |
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| Finger, F. | Author |
| Year | 2010 (April) | Volume | 74 |
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| Issue | 2 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/minmag.2010.073.2.217Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 244059 | Long-form Identifier | mindat:1:5:244059:4 |
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| GUID | 0 |
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| Full Reference | Krenn, E., Finger, F. (2010) 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. Mineralogical Magazine, 74 (2) 217-225 doi:10.1180/minmag.2010.073.2.217 |
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| Plain Text | Krenn, E., Finger, F. (2010) 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. Mineralogical Magazine, 74 (2) 217-225 doi:10.1180/minmag.2010.073.2.217 |
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| In | (2010, April) Mineralogical Magazine Vol. 74 (2) Mineralogical Society |
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| Abstract/Notes | AbstractAccessory monazite-(Ce) with an extraordinarily high proportion of the xenotime component in solid solution of 21–42 mol.% (6.5–14 wt.% Y2O3, 6–11 wt.% HREE2O3) was discovered in a retrogressed Variscan high-pressure, high-temperature granulite from the southern Bohemian Massif, Austria. The grains with the highest proportion of xenotime (XXno ~0.4) should have had a minimum formation temperature of ~1050°C, according to published monazite-xenotime miscibility gap thermometers. This high temperature is consistent with previous petrological studies on the south Bohemian granulites indicating ~1000°C/16 kbar for the peak metamorphic stage. |
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