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Mckelveyite group minerals – Part 2: Alicewilsonite-(YCe), Na2Sr2YCe(CO3)6 ⋅ 3H2O, a new species
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Abstract. The new mckelveyite group mineral alicewilsonite-(YCe),
ideally Na2Sr2YCe(CO3)6 ⋅ 3H2O, was found
at Mont Saint-Hilaire, Quebec, Canada, and subsequently at the Saint-Amable
sill, Quebec, Canada, and the Khibiny Massif, Kola Peninsula, Russia.
Alicewilsonite-(YCe) crystals are commonly hemimorphic pseudotrigonal and
pseudohexagonal and show barrel-shaped, saucer-shaped, spindle-shaped,
cone-shaped, columnar, tabular, and platy habits. They are usually up to 2–3 mm in size with some larger crystals reaching 2–3 cm. The crystals often
form stacked or parallel growth aggregates and rosettes.
Alicewilsonite-(YCe) colour varies from pale yellow to yellow, lemon yellow,
green yellow, orange-yellow, pale green to green, pale grey to grey, green
grey, beige, and colourless. The streak is white; the lustre is vitreous.
The cleavage is fair to indistinct, parallel to (001). The Mohs hardness is
3. Dcalc is 3.37 g cm−3. Alicewilsonite-(YCe) is optically biaxial
(+), with α=1.554(3), β=1.558(3), γ=1.644(2), 2V (calc.) = 26∘, 2V (meas.) = 20(3)∘ (589 nm).
The IR spectrum is reported. The
composition (wt %, average of six analyses) is Na2O 7.42, CaO 0.72,
SrO 21.49, BaO 1.41, Y2O3 8.52, La2O3 5.93,
Ce2O3 9.52, Pr2O3 0.59, Nd2O3 1.75,
Sm2O3 0.46, Gd2O3 0.83, Dy2O3 1.65,
Ho2O3 0.34, Er2O3 1.21, Yb2O3 0.64, CO2
29.33, H2O 6.13, total 97.94. The empirical formula of the holotype
calculated on the basis of six cations is
Na2.11Ca0.11Sr1.83Ba0.08Y0.67(Ce0.51La0.32Pr0.03Nd0.09Sm0.02Gd0.04
Dy0.08Ho0.02Er0.06Yb0.03)Σ1.20(CO3)5.88 (H2O)3.00.
The mineral is triclinic,
P1, a=9.0036(6) Å, b=9.0175(6) Å, c=6.7712(5) Å, α=102.724(2)∘, β=116.398(2)∘, γ=60.003(2)∘, V=426.46(5) Å3,
and Z=1. The strongest
reflections of the powder X-ray diffraction pattern [d,Å(I)(hkl)] are
6.07(31)(001), 4.372(100)(120, 2‾1‾1, 11‾0), 4.037(25)(1‾11, 1‾2‾1, 210),
3.201(25)(121, 2‾1‾2, 11‾1),
2.831(67)(1‾12, 1‾2‾2, 211, 1‾21, 21‾0), 2.601(39)(030, 3‾3‾1,3‾01), 2.236(24)(2‾4‾1, 2‾21,
4‾2‾1). 2.019(23)(003, 2‾22, 2‾4‾2‾, 420). 1.9742(24)(032, 3‾03,
3‾3‾3, 331, 03‾2, 301). The crystal
structure, solved and refined from single-crystal X-ray diffraction data
(R1=0.055), is of the weloganite type.
Title: Mckelveyite group minerals – Part 2: Alicewilsonite-(YCe), Na2Sr2YCe(CO3)6 ⋅ 3H2O, a new species
Description:
Abstract.
The new mckelveyite group mineral alicewilsonite-(YCe),
ideally Na2Sr2YCe(CO3)6 ⋅ 3H2O, was found
at Mont Saint-Hilaire, Quebec, Canada, and subsequently at the Saint-Amable
sill, Quebec, Canada, and the Khibiny Massif, Kola Peninsula, Russia.
Alicewilsonite-(YCe) crystals are commonly hemimorphic pseudotrigonal and
pseudohexagonal and show barrel-shaped, saucer-shaped, spindle-shaped,
cone-shaped, columnar, tabular, and platy habits.
They are usually up to 2–3 mm in size with some larger crystals reaching 2–3 cm.
The crystals often
form stacked or parallel growth aggregates and rosettes.
Alicewilsonite-(YCe) colour varies from pale yellow to yellow, lemon yellow,
green yellow, orange-yellow, pale green to green, pale grey to grey, green
grey, beige, and colourless.
The streak is white; the lustre is vitreous.
The cleavage is fair to indistinct, parallel to (001).
The Mohs hardness is
3.
Dcalc is 3.
37 g cm−3.
Alicewilsonite-(YCe) is optically biaxial
(+), with α=1.
554(3), β=1.
558(3), γ=1.
644(2), 2V (calc.
) = 26∘, 2V (meas.
) = 20(3)∘ (589 nm).
The IR spectrum is reported.
The
composition (wt %, average of six analyses) is Na2O 7.
42, CaO 0.
72,
SrO 21.
49, BaO 1.
41, Y2O3 8.
52, La2O3 5.
93,
Ce2O3 9.
52, Pr2O3 0.
59, Nd2O3 1.
75,
Sm2O3 0.
46, Gd2O3 0.
83, Dy2O3 1.
65,
Ho2O3 0.
34, Er2O3 1.
21, Yb2O3 0.
64, CO2
29.
33, H2O 6.
13, total 97.
94.
The empirical formula of the holotype
calculated on the basis of six cations is
Na2.
11Ca0.
11Sr1.
83Ba0.
08Y0.
67(Ce0.
51La0.
32Pr0.
03Nd0.
09Sm0.
02Gd0.
04
Dy0.
08Ho0.
02Er0.
06Yb0.
03)Σ1.
20(CO3)5.
88 (H2O)3.
00.
The mineral is triclinic,
P1, a=9.
0036(6) Å, b=9.
0175(6) Å, c=6.
7712(5) Å, α=102.
724(2)∘, β=116.
398(2)∘, γ=60.
003(2)∘, V=426.
46(5) Å3,
and Z=1.
The strongest
reflections of the powder X-ray diffraction pattern [d,Å(I)(hkl)] are
6.
07(31)(001), 4.
372(100)(120, 2‾1‾1, 11‾0), 4.
037(25)(1‾11, 1‾2‾1, 210),
3.
201(25)(121, 2‾1‾2, 11‾1),
2.
831(67)(1‾12, 1‾2‾2, 211, 1‾21, 21‾0), 2.
601(39)(030, 3‾3‾1,3‾01), 2.
236(24)(2‾4‾1, 2‾21,
4‾2‾1).
2.
019(23)(003, 2‾22, 2‾4‾2‾, 420).
1.
9742(24)(032, 3‾03,
3‾3‾3, 331, 03‾2, 301).
The crystal
structure, solved and refined from single-crystal X-ray diffraction data
(R1=0.
055), is of the weloganite type.
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