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Lukechangite-(Ce) Abstracted by Malcolm Back
The specimens were collected from a large pegmatite dyke in the nepheline syenite intrusion. The associated minerals are microcline, analcime, sodalite, aegerine, serandite, eudialyte, catapleiite, fluorite, petersenite-(Ce), siderite, astrophyllite, and albite. Horvathite-(Y), UK96, and UK93 were found in a different section of the same pegmatite, and the assemblage is thought to be a late-stage pegmatite. Lukechangite-(Ce) has two distinct habits: 1) tabular, 0.5 to 1.0 mm. and 2) short prismatiuc to barrel-shaped crystals, 0.5 to 1.0 mm. across. The forms include {0001}, {11(bar2)0} and {11(bar2)1} plus at least one more bipyramid. Striations parallel {0001} are due to oscillatory growth of the bipyramid. Lukechangite-(Ce) is colourless to pale beige with a white streak and vitreous lustre, somewhat pearly on {0001}. Hardness is ~4½ (Mohs scale), brittle with an uneven to conchoidal fracture and with perfect {0001} cleavage. It does not fluoresce. The calculated density is 4.02 g/cm3, and is soluble in 1:1 HCl with effervescence. Lukechangite-(Ce) is uniaxial negative, w = 1.728(3) and e = 1.542(1) (l = 589 nm). It is hexagonal, space group P63/mmc, a 5.0612(8), c 22.820(9) Å, V = 509(1) Å, and Z = 2.
Source:Grice, J.D. and Chao, G.Y. 1997. Lukechangite-(Ce) a new rare-earth-fluorocarbonate mineral from Mont Saint-Hilaire, Québec. Amer. Min. 82:1255-1260.
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