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EntityQ3801840· pop 12· linked from 7 articles

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).

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

Named after
Iran
Image
Phoenicochroite, Iranite-235291.jpg
Show 8 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
streak color
yellow
type locality (geology)
Anarak District
IMA Mineral Symbol
Irn
Strunz 8th edition (series ID, updated)
VI/E.02 – Anhang

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Encyclopedic overview

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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.

Excerpted from Wikipedia’s “iranite” article, available under the CC BY-SA 4.0 licence.

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