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The Canadian Mineralogist; April 2008; v. 46; no. 2; p. 413-422; DOI: 10.3749/canmin.46.2.413
© 2008 Mineralogical Association of Canada
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Articles

TUNDRITE-(Ce) FROM MONT SAINT-HILAIRE, QUEBEC: CRYSTAL-STRUCTURE ANALYSIS AND SPECIES CHARACTERIZATION

Joel D. Grice1,§, Ralph Rowe1, Glenn Poirier1 and Quintin Wight2

1 Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada
2 525 Fielding Drive, Ottawa, Ontario K1V 7G7, Canada

§ E-mail address: jgrice{at}mus-nature.ca

Tundrite-(Ce), ideally Na2Ce2TiO2(SiO4)(CO3)2, has been found recently in the Mont Saint-Hilaire quarry, Quebec. It occurs as yellow-green, bladed, singly terminated crystals up to 9 mm in length. Minerals associated with tundrite-(Ce) are aegirine, analcime, an astrophyllite-group mineral, catapleiite, a eudialyte-group mineral, gonnardite, mangan-neptunite, monazite-(Ce), natrolite, rhodochrosite, sphalerite and vinogradovite. Tundrite-(Ce) is triclinic, space group PFormula, with the following unit-cell parameters, refined from powder-diffraction data: a 7.5702(6), b 13.949(2), c 5.0235(5) Å, {alpha} 100.19(1), β 70.88(1), {gamma} 101.26(1)°, V 487.91(6) Å3 and Z = 2. Crystals are tabular on {010} and elongate on [001], with pinacoid forms: {100}, {010}, {201} and {Formula01}. Electron-microprobe analyses give the average and ranges: Na2O 9.44 (9.07–9.66), CaO 0.34 (0.16–0.42), La2O3 16.12 (15.26–17.95), Ce2O3 27.01 (25.41–28.56), Pr2O3 2.13 (1.72–2.38), Nd2O3 6.16 (5.61–6.58), Sm2O3(0.38 (0.18–0.73), TiO2 11.17 (10.73–11.93), Nb2O5 2.30 (1.14–3.11), Ta2O5 0.07 (0.00–0.15), SiO2 9.32 (9.10–9.54), CO2 13.91 (TGA), H2O 0.36 (TGA), for a total of 98.80 (97.43–100.17) wt.%. The empirical formula based on the crystal-structure analysis, ideally showing 24 oxygen atoms, is 2[(Na1.906Ca0.039) {Sigma}1.945 (Ce1.030La0.621Nd0.229Pr0.081Sm0.014) {Sigma}1.975 (Ti0.875Nb0.109) {Sigma}0.984O2H0.250 (Si0.971O4)(C0.989O3)2]. The structure has been refined to an R index of 2.7% for 2827 unique reflections. The structure has three chemically distinct layers parallel to (010): (1) a Na–Ti–Si–O slab, (2) a Ce–C–O slab and (3) a Na–O slab. Slabs are cross-linked by independent [CO3]2– and [SiO4]4– groups. Minor amounts of OH are present to ensure charge balance as a result of the substitutions Nb {leftrightarrow} Ti and Ca {leftrightarrow} REE.

Keywords: tundrite-(Ce), crystal structure, rare-earth elements, chemical composition, infrared spectroscopy, hydrogen, Mont Saint-Hilaire, Quebec.







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