| Reference Type | Journal (article/letter/editorial) |
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| Title | Xenotime-(Y) and Sn-rich thortveitite in miarolitic pegmatites from Baveno, Southern Alps, Italy |
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| Journal | Mineralogical Magazine |
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| Authors | Guastoni, A. | Author |
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| Nestola, F. | Author |
| Ferraris, C. | Author |
| Parodi, G. | Author |
| Year | 2012 (June) | Volume | 76 |
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| Issue | 3 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/minmag.2012.076.3.23Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 244249 | Long-form Identifier | mindat:1:5:244249:9 |
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| GUID | 0 |
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| Full Reference | 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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| Plain Text | 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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| Abstract/Notes | AbstractXenotime-(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. |
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