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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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Reference TypeJournal (article/letter/editorial)
TitleZr-rich non metamict perrierite-(Ce) from holocrystalline ejecta in the Sabatini volcanic complex (Latium, Italy)
JournalMineralogical MagazineISSN0026-461X
AuthorsParodi, G. C.Author
Della Ventura, G.Author
Mottana, A.Author
Raudsepp, M.Author
Year1994 (December)Volume58
Issue393
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_58/58-393-607.pdf+
DOIdoi:10.1180/minmag.1994.058.393.09Search in ResearchGate
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Mindat Ref. ID2085Long-form Identifiermindat:1:5:2085:9
GUID0
Full ReferenceParodi, 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
Plain TextParodi, 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
In(1994, December) Mineralogical Magazine Vol. 58 (393) Mineralogical Society
Abstract/NotesAbstractThis 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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Locality Pages

LocalityCitation Details
La Mola, Anguillara Sabazia, Metropolitan City of Rome Capital, Lazio, Italy

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MineralCitation Details
Perrierite-(Ce)

Mineral Occurrences

LocalityMineral(s)
La Mola, Anguillara Sabazia, Metropolitan City of Rome Capital, Lazio, Italy Baddeleyite, Biotite, Clinopyroxene Subgroup, Perrierite-(Ce), Sanidine, Titanite, Zircon


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