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Barikaite, Pb (sub 10) Ag (sub 3) (Sb (sub 8) As (sub 11) ) (sub Sigma 19) S (sub 40) , a new member of the sartorite homologous series

D. Topa, E. Makovicky, H. Tajedin, H. Putz and G. Zagler
Barikaite, Pb (sub 10) Ag (sub 3) (Sb (sub 8) As (sub 11) ) (sub Sigma 19) S (sub 40) , a new member of the sartorite homologous series
Mineralogical Magazine (October 2013) 77 (7): 3039-3046

Abstract

Barikaite, ideally Pb (sub 10) Ag (sub 3) (Sb (sub 8) As (sub 11) ) (sub Sigma 19) S (sub 40) , is a new mineral species from the Barika Au-Ag deposit, Azarbaijan Province, western Iran. It was formed in fractures developed in silica bands situated in massive banded pyrite and baryte ores. These fractures house veinlets that contain a number of Ag-As-Sb-Pb-rich sulfosalts, tetrahedrite-tennantite, realgar, pyrite and electrum. Barikaite appears as inclusions in guettardite. The mineral is opaque, greyish black with a metallic lustre; it is brittle without any discernible cleavage. In reflected light barikaite is greyish white, pleochroism is distinct, white to dark grey. Internal reflections are absent. In crossed polars, anisotropism is distinct with rotation tints in shades of grey. The reflectance data (%, in air) are: 37.0, 39.3 at 470 nm, 34.1, 36.9 at 546 nm, 33.1, 36.2 at 589 nm and 31.3, 34.1 at 650 nm. The Mohs hardness is 3-3 1/2, microhardness VHN (sub 50) exhibits the range 192-212, with a mean value of 200 kg mm (super -2) . The average results of five electron-microprobe analyses in a grain are (in wt.%): Pb 35.77(33), Ag 5.8(1), Tl 0.15(08), Sb 18.33(09), As 15.64(16), S 24.00(15), total 99.69(10) wt.%, corresponding to Pb (sub 9.31) Ag (sub 2.90) Tl (sub 0.04) (Sb (sub 8.12) As (sub 11.26) ) (sub Sigma 19.36) S (sub 40.37) (on the basis of 32Me + 40S = 72 a.p.f.u.). The simplified formula, Pb (sub 10) Ag (sub 3) (Sb (sub 8) As (sub 11) ) (sub Sigma 19) S (sub 40) , is in accordance with the results of a crystal-structure analysis, and requires Pb 37.89, Ag 5.91, Sb 17.79, As 15.05 and S 23.42 (wt.%). The variation of chemical composition is minor, the empirical formula ranging from Pb (sub 10.39) Ag (sub 2.32) Tl (sub 0.02) Sb (sub 7.52) As (sub 11.27) S (sub 40.49) to Pb (sub 9.24) Ag (sub 2.93) Tl (sub 0.04) Sb (sub 8.13) As (sub 11.35) S (sub 40.31) . Barikaite has monoclinic symmetry, space group P2 (sub 1) /n and unit-cell parameters a 8.5325(7) Aa, b 8.0749(7) Aa, c 24.828(2) Aa, and beta 99.077(6) degrees , Z = 1. Calculated density for the empirical formula is 5.34 (g cm (super -3) ). The strongest eight lines in the (calculated) powder-diffraction pattern [d in Aa(I)(hkl)] are: 3.835(63)(022), 3.646(100)(016), 3.441(60)(212), 3.408(62)(2I14), 2.972(66)(2I16), 2.769(91)(222), 2.752(78)(4I24) and 2.133(54)(402). Barikaite is the N = 4 member of the sartorite homologous series with a near-equal role of As and Sb, which have an ordered distribution pattern in the structure. It is a close homeotype of rathite and more distantly related to dufrenoysite (both distinct, pure arsenian N = 4 members) and it completes the spectrum of Sb-rich members of the sartorite homologous series. The new mineral and its name have been approved by the IMA-CNMNC (IMA 2012-055).


ISSN: 0026-461X
EISSN: 1471-8022
Coden: MNLMBB
Serial Title: Mineralogical Magazine
Serial Volume: 77
Serial Issue: 7
Title: Barikaite, Pb (sub 10) Ag (sub 3) (Sb (sub 8) As (sub 11) ) (sub Sigma 19) S (sub 40) , a new member of the sartorite homologous series
Affiliation: Natural History Museum Vienna, Vienna, Austria
Pages: 3039-3046
Published: 201310
Text Language: English
Publisher: Mineralogical Society, London, United Kingdom
References: 29
Accession Number: 2013-091423
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables
N36°00'00" - N42°00'00", E44°04'60" - E50°00'00"
Secondary Affiliation: University of Copenhagen, DNK, DenmarkTarbiat Modares University, IRN, IranUniversity of Salzburg, AUT, Austria
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: 201353
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