Ardaite | |
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General | |
Category | Sulfosalt minerals, Lead minerals |
Formula (repeating unit) | Pb19Sb13S35Cl7 |
IMA symbol | Ada[1] |
Strunz classification | 2.LB.30 (10 ed) 2/E.19-20 (8 ed) |
Dana classification | 02.15.01.01 |
Crystal system | Monoclinic Unknown space group |
Identification | |
Color | Greenish gray or bluish green |
Mohs scale hardness | 2.5-3 |
Luster | Metallic |
Density | 6.44 |
Pleochroism | Weak |
References | Breskovska, V. V.; Mozgova, N. N.; Bortnikov, N. S.; Gorshkov, A. I.; Tzepin, A. I. (1982), "Ardaite, a new lead-antimony chlorsulphosalt" (PDF), Mineral. Mag., 46 (340): 357–361, Bibcode:1982MinM...46..357B, doi:10.1180/minmag.1982.046.340.10, S2CID 128756669 |
Ardaite is a very rare sulfosalt mineral with chemical formula Pb19Sb13S35Cl7 in the monoclinic crystal system,[2][3] named after the Arda River, which passes through the type locality.[4] It was discovered in 1978 and approved by the International Mineralogical Association in 1980.[5][6][7] It was the second well-defined natural chlorosulfosalt, after dadsonite.[8]
Greenish gray or bluish green in color, its luster is metallic. Ardaite occurs as 50 μm fine-grained aggregates of acicular crystals associated with galena, pyrostilpnite, anglesite, nadorite, and chlorine-bearing robinsonite and semseyite, in the Madjarovo polymetallic ore deposit in Bulgaria. Ardaite has a hardness of 2.5 to 3 on Mohs scale and a density of approximately 6.44.[2]
The type locality is the Madjarovo polymetallic ore deposit in the Rhodope Mountains.[9][10] Later its occurrence was proved in the Gruvåsen deposit, near Filipstad, Bergslagen, Sweden.[6]