Iranite | |
---|---|
General | |
Category | Silicate mineral |
Formula (repeating unit) | Pb10Cu(CrO4)6(SiO4)2(F,OH)2 |
IMA symbol | Irn[1] |
Strunz classification | 7.FC.15 |
Crystal system | Triclinic |
Space group | Triclinic pedial H-M symbol: (1) Space group: P1 |
Unit cell | a = 10.02 Å, b = 9.54 Å, c = 9.89 Å; α = 104.5°, β = 66°, γ = 108.5°; Z=1 |
Identification | |
Color | Brown to orange |
Crystal habit | Equant to flattened euhedral crystals |
Mohs scale hardness | 3 |
Luster | Vitreous |
Streak | Yellow |
Specific gravity | 5.8 |
Optical properties | Biaxial |
Refractive index | nα = 2.250 - 2.300 nγ = 2.400 - 2.500 |
Birefringence | δ = 0.150 - 0.200 |
References | [2][3][4] |
Iranite (Persian: ایرانیت) is a triclinic lead copper chromate silicate mineral with formula Pb10Cu(CrO4)6(SiO4)2(F,OH)2. It was first described from an occurrence in Iran. It is the copper analogue of hemihedrite (Pb10Zn(CrO4)6(SiO4)2(F,OH)2).[3]
It occurs as an oxidation product of hydrothermal lead-bearing veins. Associated minerals include dioptase, fornacite, wulfenite, mimetite, cerussite and diaboleite.[2] It was first described in 1970 for an occurrence in the Sebarz Mine, northeast of Anarak, Iran.[3][2]
References
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- 1 2 3 Handbook of Mineralogy
- 1 2 3 Mindat page for Iranite
- ↑ Webmineral data for Iranite
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