
wurtzite
Sign in to saveWurtzite is a zinc and iron sulfide mineral with the chemical formula , a less frequently encountered structural polymorph form of sphalerite. The iron content is variable up to eight percent. It is trimorphous with matraite and sphalerite.
Key facts
- Mineral.class
- Dihexagonal pyramidal (6mm) H-M symbol: (6mm)
- Mineral.symmetry
- P63mc
- Mineral.color
- Brownish black, orange brown, reddish brown, black
- Mineral.habit
- Radial clusters and colloform crusts and masses. Also as tabular crystals
- Mineral.cleavage
- [110] and [0001]
- Mineral.fracture
- Uneven – irregular
- Mineral.mohs
- 3.5–4
- Mineral.luster
- Resinous, brilliant submetallic on crystal faces
- Mineral.refractive
- nω = 2.356 nε = 2.378
- Mineral.opticalprop
- Uniaxial (+)
- Mineral.birefringence
- δ = 0.022
- Mineral.streak
- light brown
- Mineral.gravity
- 4.09 measured, 4.10 calculated
- Mineral.diaphaneity
- Translucent
- Mineral.other
- Nonmagnetic, non-radioactive
- Mineral.SMILES
- [ZnH2-2]1[S+2]47[ZnH-2]2[S+2][ZnH-2]3[S+2]8([ZnH2-2][SH+2]([ZnH2-2]4)[ZnH2-2]6)[ZnH-2]4[S+2][ZnH-2]5[S+2]6([ZnH2-2]6)[Zn-2]78[S+2]78[ZnH-2]([SH+2]69)[SH+2]5[ZnH2-2][SH+2]4[ZnH-2]7[SH+2]3[ZnH2-2][SH+2]2[ZnH-2]8[SH+2]1[ZnH2-2]9
- Mineral.Jmol
- [ZnH2-2]1[SH+2]([ZnH2-2]6)[ZnH2-2][SH+2]7[ZnH-2]2[S+2][Zn-2]3([S+2][ZnH-2]9[S+2]5)[S+2]18[Zn-2]45[S+2][ZnH-2]5[SH+2]6[Zn-2]78[S+2]78[ZnH2-2][SH+2]5[ZnH2-2][S+2]4([ZnH2-2][SH+2]9[ZnH2-2]4)[ZnH-2]7[S+2]34[ZnH2-2][SH+2]2[ZnH2-2]8
- Mineral.name
- Wurtzite
via Wikipedia infobox
Wikidata facts
- Image
- Wurtzite6779.jpg
Show 6 more facts
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 2.CB.45
- chemical formula
- ZnS
- Nickel-Strunz 9th edition (updated 2009)
- 2.CB.45
- Commons category
- Wurtzite
- IMA Mineral Symbol
- Wur
- Strunz 8th edition (series ID, updated)
- II/B.06
Sources (1)
via Wikidata · CC0
~2 min read
Article
4 sectionsContents
- Structure
- See also
- References
- External links
Wurtzite is a zinc and iron sulfide mineral with the chemical formula , a less frequently encountered structural polymorph form of sphalerite. The iron content is variable up to eight percent. It is trimorphous with matraite and sphalerite.
It occurs in hydrothermal deposits associated with sphalerite, pyrite, chalcopyrite, barite and marcasite. It also occurs in low-temperature clay-ironstone concretions.
Gallery (2)
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