Reference Type | Journal (article/letter/editorial) |
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Title | Zr-rich non metamict perrierite-(Ce) from holocrystalline ejecta in the Sabatini volcanic complex (Latium, Italy) |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Parodi, G. C. | Author |
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Della Ventura, G. | Author |
Mottana, A. | Author |
Raudsepp, M. | Author |
Year | 1994 (December) | Volume | 58 |
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Issue | 393 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_58/58-393-607.pdf+ |
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DOI | doi:10.1180/minmag.1994.058.393.09Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 2085 | Long-form Identifier | mindat:1:5:2085:9 |
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GUID | 0 |
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Full Reference | Parodi, G. C., Della Ventura, G., Mottana, A., Raudsepp, M. (1994) Zr-rich non metamict perrierite-(Ce) from holocrystalline ejecta in the Sabatini volcanic complex (Latium, Italy) Mineralogical Magazine, 58 (393) 607-613 doi:10.1180/minmag.1994.058.393.09 |
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Plain Text | Parodi, G. C., Della Ventura, G., Mottana, A., Raudsepp, M. (1994) Zr-rich non metamict perrierite-(Ce) from holocrystalline ejecta in the Sabatini volcanic complex (Latium, Italy) Mineralogical Magazine, 58 (393) 607-613 doi:10.1180/minmag.1994.058.393.09 |
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In | (1994, December) Mineralogical Magazine Vol. 58 (393) Mineralogical Society |
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Abstract/Notes | AbstractThis paper reports the first in-situ finding of perrierite-(Ce) in Latium. The mineral occurs as brownish-red, transparent, well-developed, euhedral, prismatic crystals inside the miarolitic cavities of a holocrystalline ejectum from La Mola, Monti dell'Anguillara district, Sabatini volcanic complex.The cell parameters (from Gandolfi film) are (in Å): a = 13.629(9), b = 5.727(1), c = 11.715(6), β(°) = 113.74(2), V(Å3) = 835.5(9). The crystal-chemical formula, based on microprobe analysis of one grain, is:This perrierite is the most Zr-rich described so far. The entry of Zr in the C site of the structure is related to the substitution of large amounts of Ca in the A site, according to the charge balancing relationship:The genesis of perrierite-(Ce) from La Mola is linked to late pneumatolitic-pegmatitic hypabyssal stages of the regional volcanic activity. |
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