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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

Luca Bindi, Fabrizio Nestola, A. Guastoni, L. Peruzzo, M. Ecker, R. Carampin and Stuart J. Mills
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

Abstract

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.


ISSN: 0026-461X
EISSN: 1471-8022
Coden: MNLMBB
Serial Title: Mineralogical Magazine
Serial Volume: 76
Serial Issue: 5
Title: 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
Affiliation: Universita di Firenze, Dipartimento di Scienze della Terra, Florence, Italy
Pages: 1153-1163
Published: 201210
Text Language: English
Publisher: Mineralogical Society, London, United Kingdom
References: 18
Accession Number: 2013-002498
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 6 tables
N46°19'60" - N46°25'00", E08°05'60" - E08°13'60"
Secondary Affiliation: Istituto di Geoscienze e Georisorse, ITA, ItalyUniversita di Padova, ITA, Italy
Country of Publication: United Kingdom
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, Copyright, Mineralogical Society of Great Britain and Ireland. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201302
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