iranite
Sign in to saveIranite (Persian: ایرانیت) is a triclinic lead copper chromate 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).
Key facts
- Mineral.name
- Iranite
- Mineral.image
- Phoenicochroite, Iranite-235291.jpg
- Mineral.imagesize
- 260px
- Mineral.category
- Chromate minerals
- Mineral.formula
- Pb10Cu(CrO4)6(SiO4)2(F,OH)2
- Mineral.IMAsymbol
- Irn
- Mineral.strunz
- 7.FC.15
- Mineral.symmetry
- Triclinic pedialH-M symbol: (1) Space group: P1
- Mineral.unit cell
- a = 10.02 Å, b = 9.54 Å, c = 9.89 Å; α = 104.5°, β = 66°, γ = 108.5°; Z = 1
- Mineral.color
- Brown to orange
- Mineral.habit
- Equant to flattened euhedral crystals
- Mineral.system
- Triclinic
- Mineral.mohs
- 3
- Mineral.luster
- Vitreous
- Mineral.streak
- Yellow
- Mineral.gravity
- 5.8
- Mineral.opticalprop
- Biaxial
- Mineral.refractive
- nα = 2.250 – 2.300 nγ = 2.400 – 2.500
via Wikipedia infobox
Wikidata facts
- Image
- Phoenicochroite, Iranite-235291.jpg
Show 5 more facts
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 7.FC.15
- Nickel-Strunz 9th edition (updated 2009)
- 7.FC.15
- Commons category
- Iranite
- IMA Mineral Symbol
- Irn
- Strunz 8th edition (series ID, updated)
- VI/E.02 – Anhang
via Wikidata · CC0
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Article
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Iranite (Persian: ایرانیت) is a triclinic lead copper chromate 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).
It occurs as an oxidation product of hydrothermal lead-bearing veins. Associated minerals include dioptase, fornacite, wulfenite, mimetite, cerussite and diaboleite. It was first described in 1970 for an occurrence in the Sebarz Mine, northeast of Anarak, Iran.