Aluminotaipingite-(CeCa), (Ce6Ca3)Al(SiO4)3[SiO3(OH)]4F3, a new member of the cerite-supergroup minerals

Aluminotaipingite-(CeCa), (Ce6Ca3)Al(SiO4)3[SiO3(OH)]4F3, is a new member of the cerite-supergroupminerals, whose general chemical formula is A9XM[TO3Ø]7Z3, (A = REE, Ca, Sr, Na, and ?; X = ?, Ca, Na,and Fe2+; M = Mg, Fe2+, Fe3+, Al, and Mn; T = Si and P; Ø = O and OH; Z = ?, OH, and F). It was found incavities of a leucogranitic orthogneiss at the Casette quarry, Montoso, Bagnolo Piemonte, CuneoProvince, Piedmont, Italy. Crystals of aluminotaipingite-(CeCa) are light pink to pink, transparent orsemitransparent, with vitreous lustre. It forms pyramidal crystals up to 0.07 mm in size and observedforms are {0 0 1}, {1 0 -2}. Tenacity is brittle, no distinct cleavage is observed, fracture is uneven. Themineral does not fluoresce in long- or short-wave ultraviolet light. The streak is white. Hardness (Mohs)= 5. The calculated density is 4.476 g cm-3.The mineral is trigonal, space group R3c, with a = 10.658(3), c = 37.865(9) Å, V = 3725(2) Å3 and Z = 6.The eight strongest X-ray powder diffraction lines are [dobs, Å (I, %) (hkl)]: 8.38(29)(0 1 2), 4.499(28)(20 2), 3.282(41)(2 1 4), 2.936(100)(0 2 10), 2.816(51)(1 2 8), 2.669(37)(2 2 0), 2.207 (29)(3 0 12) and1.935(35)(2 3 8). The structure was refined to R =0.0306 for 2297 reflections with I >2?(I). The crystalstructure of aluminotaipingite-(CeCa) contains two nine-fold coordinated sites (A1 and A2), which aremainly occupied by lanthanides, and a third nine-fold coordinated A3 site containing almost equalamounts of lanthanides and Ca. The X site is vacant and at the octahedral M site aluminium prevailsupon Fe3+. Among the three independent T sites, T2 belongs to a (SiO4)4- anion, whereas T1 and T3 to(SiO3OH)3- anions. Fluorine is involved in coordination with the A1 and A3 sites.