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European Journal of Mineralogy; January, February 2007; v. 19; no. 1; p. 95-103; DOI: 10.1127/0935-1221/2007/0019-0095
© 2007 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Fluorcalciobritholite, (Ca,REE)5[(Si,P)O4]3F, a new mineral: description and crystal chemistry

Igor V. Pekov1, Marco Pasero2,*, Asiya N. Yaskovskaya3, Nikita V. Chukanov4, Dmitry Yu. Pushcharovsky1, Stefano Merlino2, Natalia V. Zubkova1, Natalia N. Kononkova5, Yury P. Men’shikov6 and Aleksandr E. Zadov7

1 Faculty of Geology, Moscow State University, Vorobievy Gory, 119992 Moscow, Russia
2 Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 53, 56126 Pisa, Italy
3 Fersman Mineralogical Museum, Leninskiy prospect 18-2, 117901 Moscow, Russia
4 Institute of Problems of Chemical Physics, 142432 Chernogolovka, Moscow Oblast, Russia
5 Institute of Geochemistry and Analytical Chemistry, Kosygin ul. 19, 117975 Moscow, Russia
6 Geological Institute of Kola Science Centre, Fersman ul. 14, 184200 Apatity, Murmansk Oblast, Russia
7 NPO Regenerator, 3rd Passage of Mar’ina Roshcha 40, 127018 Moscow, Russia

* Corresponding author, e-mail: pasero{at}dst.unipi.it

The new mineral fluorcalciobritholite, ideally Ca3Ce2(SiO4)2(PO4)F, has been found at Mount Kukisvumchorr, Khibiny alkaline complex, Kola Peninsula, Russia, in veinlets which contains aggregates of orthoclase, nepheline, sodalite and biotite in association with grains of fayalite, gadolinite-(Ce), zircon, monazite-(Ce), zirconolite ("polymignite"), fluorapatite, fluorite, molybdenite, löllingite and graphite. Fluorcalciobritholite forms long-prismatic hexagonal crystals up to 0.5 x 10 mm; the main crystal form is the hexagonal prism {10–10}. The mineral is transparent, with a pale pinkish to brown colour and a white streak. The hardness (Mohs) is 5.5, and the observed density is 4.2(1) g/cm3. Optically, it is uniaxial (–) with {omega} 1.735(5), {varepsilon} 1.730(5). Electron microprobe gave the following empirical formula based on [Si+P+S] = 3 apfu: [Ca2.80 (Ce0.93La0.54Nd0.26Y0.18Pr0.08Sm0.03Gd0.03Dy0.02Yb0.02Er0.01){sum}2.12 Th0.04Mn0.03 Sr0.02] {sum}4.99 [(Si1.94P1.06) {sum}3O12] [F0.76O0.22Cl0.01]{sum}0.99 (Z = 2). The IR spectrum of metamict fluorcalciobritholite from Siberia showed a marked similarity with those of hydroxylbritholite-(Ce) and hydroxylbritholite-(Y). The strongest lines of the X-ray powder pattern [d in Å (I) (hkl)] are: 3.51 (45) 002, 3.15 (70) 102, 2.85 (100) 211, 121, 2.78 (60) 300. The mineral is hexagonal, space group P63/m, with a = 9.580(7), c = 6.985(4) Å, V = 555.2(7) Å3. The crystal structure was refined from single-crystal X-ray diffraction data to RF = 0.029. Fluorcalciobritholite, whose simplified formula is (Ca,REE)5[(Si,P)O4]3F, differs from fluorbritholite in having Ca > {sum}REE, and differs from fluorapatite in having Si > P. Its compositional field falls within the limits Ca2.5REE2.5(SiO4)2.5(PO4)0.5F (boundary with fluorbritholite) and Ca3.5REE1.5(SiO4)1.5(PO4)1.5F (boundary with fluorapatite). Both the mineral and its name have been approved by the IMA Commission on New Minerals and Mineral Names.

Key-words: fluorcalciobritholite, new mineral, crystal structure, Khibiny alkaline complex, britholite group, apatite group.







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