KUANNERSUITE-(Ce), Ba6Na2REE2(PO4)6FCl, A NEW MEMBER OF THE APATITE GROUP, FROM T
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摘要

Kuannersuite-(Ce) is a new mineral species belonging to the apatite group. It was found in the Ilímaussaq alkaline complex, South Greenland, and occurs as light rose-colored hexagonal prismatic crystals, up to 1.5 mm long, with a white streak and a vitreous luster. Associated minerals include aegirine, analcime, beryllite, chkalovite, galena, gmelinite, gonnardite, lovdarite, nabesite, neptunite, pectolite, polylithionite, pyrochlore, sphalerite and tugtupite. It is brittle with an uneven fracture, and poor {001} and {100} cleavages, and a Mohs hardness of 4½ – 5½. Although kuannersuite-(Ce) is trigonal and uniaxial negative with ε= 1.669(1) and ω = 1.694(1), it has a 2V(meas.) of 10 to 20°. The empirical formula based on results of electron-microprobe analyses and calculated with 26 anions is: (Ba5.61Sr0.15K0.03)∑5.79Na2.14(Ce1.00Nd0.43La0.25Sm0.05Th0.02Pr0.01)∑1.76 (P6.02Si0.14)∑6.16O23.72(F1.70Cl0.58)∑2.28 or, ideally, Ba6Na2REE2(PO4)6FCl. The strongest X-ray-diffraction lines [d in Å (I)(hkl)] are: 2.969(100)(211,112), 2.867(60)(300), 1.965(80)(320,213). The crystal structure was refined (R = 2.79%) in space group P3̅, with a 9.9097(6) Å, c 7.4026(6) Å, V 629.42(7) Å3, Z = 1 and Dcalc. = 4.51(1) g/cm3. Ba, REE and Na are distributed over different structural sites with distinct atomic coordinations, whereas F and Cl occupy positions in two different octahedrally coordinated voids formed by Ba atoms, with distances typical for a regular six-fold coordination of these anions. Cl is incorporated only in the larger of the two coordination polyhedra. A comparative analysis of the crystal chemistry of kuannersuite-(Ce) and related Ba and Sr phases from the apatite family is reported.

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