Ardaite

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Ardaite
Ardaite associated with galenite, Madjarovo polymetallic ore deposit, National Natural History Museum, Sofia, Bulgaria
General
CategorySulfosalt minerals, Lead minerals
Formula
(repeating unit)
Pb19Sb13S35Cl7
Strunz classification2.LB.30 (10 ed)
2/E.19-20 (8 ed)
Dana classification02.15.01.01
Crystal systemMonoclinic
Unknown space group
Identification
ColorGreenish gray or bluish green
Mohs scale hardness2.5-3
LusterMetallic
Density6.44
PleochroismWeak
ReferencesBreskovska V. V., N. N. Mozgova, N. S. Bortnikov, A. I. Gorshkov, A. I. Tzepin (1982): Ardaite, a new lead-antimony chlorsulphosalt. Mineral. Mag., 46, 357-361.

Ardaite is a very rare sulfosalt mineral with chemical formula Pb19Sb13S35Cl7 in the monoclinic crystal system,[1][2] named after the Arda river, which passes through the type locality.[3] It was discovered in 1978 and approved by the International Mineralogical Association in 1980.[4][5][6] It was the second well-defined natural chlorosulfosalt, after dadsonite.[7]

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 Cl-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.[1]

The type locality is the Madjarovo polymetallic ore deposit in the Rhodope mountains.[8][9] Later its occurrence was proved in the Gruvåsen deposit, near Filipstad, Bergslagen, Sweden.[5]

References

Paragenesis of ardaite & galena, Madjarovo ore deposit, Bulgaria, National Natural History Museum, Sofia, Bulgaria

See also

List of minerals (complete)