Raberite, Tl (sub 5) Ag (sub 4) As (sub 6) SbS (sub 15) , a new Tl-bearing sulfosalt from Lengenbach Quarry, Binn Valley, Switzerland; description and crystal structure
Raberite, Tl (sub 5) Ag (sub 4) As (sub 6) SbS (sub 15) , a new Tl-bearing sulfosalt from Lengenbach Quarry, Binn Valley, Switzerland; description and crystal structure
Mineralogical Magazine (October 2012) 76 (5): 1153-1163
- Binnental
- Central Europe
- chemical composition
- coexisting minerals
- color
- crystal structure
- electron probe data
- Europe
- formula
- lattice parameters
- metals
- new minerals
- optical properties
- physical properties
- realgar
- space groups
- sulfides
- sulfosalts
- Switzerland
- thallium
- unit cell
- Valais Switzerland
- hatchite
- smithite
- trechmannite
- edenharterite
- jentschite
- Lengenbach Quarry
- raberite
Raberite, ideally Tl (sub 5) Ag (sub 4) As (sub 6) SbS (sub 15) , is a new mineral from Lengenbach quarry in the Binn Valley, Valais, Switzerland. It occurs very rarely as euhedral crystals up to 150 mu m across associated with yellow needle-like smithite, realgar, hatchite and probable trechmannite, edenharterite, jentschite and two unidentified sulfosalts. Raberite is opaque with a metallic lustre and has a dark brown-red streak. It is brittle with a Vickers hardness (VHN (sub 10) ) of 52 kg mm (super -2) (range 50-55) corresponding to a Mohs hardness of 2 1/2-3. In reflected light raberite is moderately bireflectant and very weakly pleochroic from light grey to a slightly greenish grey. It is very weakly anisotropic with greyish to light blue rotation tints between crossed polars. Internal reflections are absent. Reflectance percentages for the four COM wavelengths [listed as R (sub min) , R (sub max) , (lambda )] are 30.6, 31.8 (471.1 nm), 28.1, 29.3 (548.3 nm), 27.1, 28.0 (586.6 nm), and 25.8, 26.9 (652.3 nm). Raberite is triclinic, space group P1i, with a = 8.920(1), b = 9.429(1), c = 20.062(3) Aa, alpha = 79.66(1), beta = 88.84(1), gamma = 62.72(1) degrees , V = 1471.6(4) Aa (super 3) and Z = 2. The crystal structure [R (sub 1) = 0.0827 for 2110 reflections with I > 2sigma (I)] consists of columns of nine-coordinate Tl atoms forming irregular polyhedra extending along [001] and forming sheets parallel to (010). The columns are decorated by corner-sharing MS (sub 3) pyramids (M = As, Sb) and linked by AgS (sub 3) triangles. Of the seven M positions, one is dominated by Sb and the others by As; the mean M-S bond distances reflect As<-->Sb substitution at these sites. The eight strongest lines in the powder diffraction pattern [d (sub calc) in Aa (I) (hkl)] are: 3.580 (100) (11i3); 3.506 (58) (1i2i3); 3.281 (73) (006); 3.017 (54) (1i23); 3.001 (98) (133); 2.657 (51) (226); 2.636 (46) (300); 2.591 (57) (330). A mean of 9 electron microprobe analyses gave Tl 39.55(13), Ag 18.42(8), Cu 0.06(2), As 17.08(7), Sb 5.61(6), S 19.15(11); total 99.87 wt.%, which corresponds to Tl (sub 4.85) Ag (sub 4.28) Cu (sub 0.02) As (sub 5.72) Sb (sub 1.16) S (sub 14.97) with 31 atoms per formula unit. The new mineral has been approved by the IMA-CNMNC Commission (IMA 2012-017) and is named for Thomas Raber, an expert on Lengenbach minerals.