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Guastoni, A., Nestola, F., Ferraris, C., Parodi, G. (2012) Xenotime-(Y) and Sn-rich thortveitite in miarolitic pegmatites from Baveno, Southern Alps, Italy. Mineralogical Magazine, 76 (3) 761-767 doi:10.1180/minmag.2012.076.3.23

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Reference TypeJournal (article/letter/editorial)
TitleXenotime-(Y) and Sn-rich thortveitite in miarolitic pegmatites from Baveno, Southern Alps, Italy
JournalMineralogical Magazine
AuthorsGuastoni, A.Author
Nestola, F.Author
Ferraris, C.Author
Parodi, G.Author
Year2012 (June)Volume76
Issue3
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2012.076.3.23Search in ResearchGate
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Mindat Ref. ID244249Long-form Identifiermindat:1:5:244249:9
GUID0
Full ReferenceGuastoni, A., Nestola, F., Ferraris, C., Parodi, G. (2012) Xenotime-(Y) and Sn-rich thortveitite in miarolitic pegmatites from Baveno, Southern Alps, Italy. Mineralogical Magazine, 76 (3) 761-767 doi:10.1180/minmag.2012.076.3.23
Plain TextGuastoni, A., Nestola, F., Ferraris, C., Parodi, G. (2012) Xenotime-(Y) and Sn-rich thortveitite in miarolitic pegmatites from Baveno, Southern Alps, Italy. Mineralogical Magazine, 76 (3) 761-767 doi:10.1180/minmag.2012.076.3.23
Abstract/NotesAbstractXenotime-(Y), (Y,REE)PO4, and thortveitite, (Sc, Y)2Si2O7, in a miarolitic cavity in a niobium, yttrium, fluorine (NYF) granitic pegmatite at Baveno, Verbania, Southern Alps, Italy, were investigated by electron microprobe analysis and single-crystal X-ray diffraction. Fluorine has an important role as a complexing agent for Y and REEs in supercritical pegmatitic fluids; annitesiderophyllite and chamosite are the most likely sources of the Y and REEs. The thortveitite from Baveno contains up to 3.20 wt.% SnO2, an unusually high Sn content. Xenotime-(Y) is enriched in Gd in comparison to other Alpine xenotimes. Quantitative chemical data and measurements of the lattice parameters show that a higher scandium content results in a smaller unit-cell volume in thortveitite. The substitution of REEs for Y up to ∼20 mol.% has little effect on the unit cell of xenotime-(Y). The textures of xenotime-(Y) and thortveitite provide information about the dissolution and crystallization processes in the miarolitic cavity.

Locality Pages

LocalityCitation Details
Baveno, Verbano-Cusio-Ossola Province, Piedmont, Italy

Mineral Pages

MineralCitation Details
Thortveitite


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