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wurtzite
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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.

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)

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Article

4 sections
Contents
  • 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.

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