Wurtzite | |
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General | |
Category | Sulfide mineral |
Formula (repeating unit) | (Zn,Fe)S |
IMA symbol | Wur |
Strunz classification | 2.CB.45 |
Dana classification | 02.08.07.01 |
Crystal system | Hexagonal |
Crystal class | Dihexagonal pyramidal (6mm) H-M symbol: (6mm) |
Space group | P63mc |
Structure | |
Jmol (3D) | Interactive image |
Identification | |
Color | Brownish black, orange brown, reddish brown, black |
Crystal habit | Radial clusters and colloform crusts and masses. Also as tabular crystals |
Cleavage | and |
Fracture | Uneven – irregular |
Mohs scale hardness | 3.5–4 |
Luster | Resinous, brilliant submetallic on crystal faces |
Streak | light brown |
Diaphaneity | Translucent |
Specific gravity | 4.09 measured, 4.10 calculated |
Optical properties | Uniaxial (+) |
Refractive index | nω = 2.356 nε = 2.378 |
Birefringence | δ = 0.022 |
Other characteristics | Nonmagnetic, non-radioactive |
References |
Wurtzite is a zinc and iron sulfide mineral with the chemical formula (Zn,Fe)S, 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.
It was first described in 1861 for an occurrence in the San José Mine, Oruro City, Cercado Province, Oruro Department, Bolivia, and named for French chemist Charles-Adolphe Wurtz. It has widespread distribution. In Europe it is reported from Příbram, Czech Republic; Hesse, Germany; and Liskeard, Cornwall, England. In the US it is reported from Litchfield County, Connecticut; Butte, Silver Bow County, Montana; at Frisco, Beaver County, Utah; and from the Joplin district, Jasper County, Missouri.
Structure
The wurtzite group includes cadmoselite (CdSe), greenockite (CdS), mátraite (ZnS), and rambergite (MnS), in addition to wurtzite.
Its crystal structure is called the wurtzite crystal structure, to which it lends its name. This structure is a member of the hexagonal crystal system and consists of tetrahedrally coordinated zinc and sulfur atoms that are stacked in an ABABABABAB pattern.
The unit cell parameters of wurtzite are (-2H polytype):
See also
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.
- ^ Handbook of Mineralogy
- ^ Wurtzite at Mindat.org
- Wurtzite at Webmineral
- Palache, Charles, Harry Berman & Clifford Frondel (1944), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume I: Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, Inc., New York. 7th edition, revised and enlarged, pp. 226-228.
- Wurtzite group on Mindat.org
- Xu, Yong-Nian; Ching, W. Y. (15 August 1993). "Electronic, optical, and structural properties of some wurtzite crystals". Physical Review B. 48 (7): 4335–4351. Bibcode:1993PhRvB..48.4335X. doi:10.1103/PhysRevB.48.4335. PMID 10008905.