Chlorbartonite, ideally K 6Fe24S26(Cl,S), is a new potassium iron sulfide chloride found as an accessory mineral in a microcline – pectolite – sodalite – aegirine vein within feldspathic urtite at Mount Koashva, Khibina massif, Kola Peninsula, Russia. The mineral occurs as roundish grains up to 2 cm across included in sodalite and natrolite crystals; it is associated with djerfish erite and rasvumite. Chlorbartonite is weakly magnetic, brittle, and has a conchoidal fracture. Cleavage and parting were not observe d. Macroscopically, the mineral is opaque, brown-black, with a black streak and submetallic luster. In reflected light, it appears optically isotropic, yellowish brown, and without internal reflections; interpolated values of reflectance ( R, %) at the standard wavelengths (nm) are: 10.8 (470), 13.5 (546), 15.1 (589), and 17.2 (650). The hardness VHN 40 is 203–212, average 207 kg/mm 2 ; the Mohs hardness is 4. The density is 3.70 g/cm 3 (measured) and 3.65 g/cm 3 (calculated). The electron-microprobe analysis of six grains gave, as an average composition: S 33.84, Cl 0.99, K 9.62, Fe 54.09, Co 0.04, Cu 0.57, total 99.15 wt.%. The empiric al formula calculated on the basis of a total of 57 atoms is K 6.08(Fe23.93Cu0.22Co0.01)� 24.16S26.00(Cl0.69S0.07)� 0.76, which yields an ideal formula of K6Fe24S26(Cl,S). The mineral is tetragonal, I4/mmm, a 10.3810(8), c 20.614(2) A, V 2221.5(3) A 3 , Z = 2. The strongest eight lines in the X-ray powder-diffraction pattern [ d in A (I)(hkl)] are: 9.25(33)(101), 5.97(65)(112), 3.121(45)(312), 2.986(100)(224), 2.380(38)(332), 2.374(57)(316), 1.834(51)(440), and 1.830(82)(408). The crystal structure has been refined to an R1 of 0.020 (447 unique observed reflections with Fo ≥ 4� Fo). The structure consists of a framework of the Fe 8S14 clusters of eight edge-sharing FeS4 tetrahedra. The framework has large cavities occupied by ClK 6 octahedra. As the name indicates, chlorbartonite is the Cl-dominant analogue of bartonite.
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