Reinerite
| Reinerite | |
|---|---|
 | |
| General | |
| Category | arsenite |
| Formula | Zn3(AsO3)2 |
| IMA symbol | Rnr[1] |
| Strunz classification | 4.JA.10 |
| Crystal system | Orthorhombic |
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Space group | Pbam (no. 55) |
| Unit cell | a = 6.092 Å, b = 14.407 Å c = 7.811 Å; Z = 4 V = 685.55 a:b:c = 0.423 : 1 : 0.542 |
| Identification | |
| Color | Sky blue, yellow green |
| Crystal habit | Rough striated pseudohexagonal crystals |
| Cleavage | Good on {110}, {011} and {111} |
| Mohs scale hardness | 5 - 5.5 |
| Luster | Vitreous to adamantine |
| Diaphaneity | Transparent |
| Specific gravity | 4.27 |
| Optical properties | Biaxial (-) |
| Refractive index | nα = 1.740 nβ = 1.790 nγ = 1.820 |
| Birefringence | Maximum δ = 0.080 |
| Other characteristics | Relief: very high |
| References | [2][3][4][5] |
Reinerite is a rare arsenite (arsenate(III)) mineral with chemical formula Zn3(AsO3)2.[3][4] It crystallizes in the orthorhombic crystal system.
Physical properties
Reinerite is most commonly found as a sky blue colored mineral, however, it may also be a light yellowish green color. Reinerite has a relative hardness of 5 to 5.5 on the Mohs Scale which is equivalent to that of a knife blade and or shard of glass. It has a density of 4.27 g/cm3,[2] and it exhibits a nonmetallic luster that may be described as glassy or vitreous.[6]
Environment
Reinerite develops in dolomite-hosted locations. It is known especially from Namibia, Africa, within the mines of Tsumeb. At the Tsumeb location, Reinerite develops within the polymetallic lead-zinc-copper deposit, 800 m (2,600 ft) below the surface, in the second oxidation zone.[5] It occurs in association with chalcocite, bornite, willemite, smithsonite, hydrozincite, hemimorphite, adamite, olivenite and gebhardite.[3]
History
Reinerite was first described in 1958 for an occurrence in the Tsumeb Mine, Tsumeb, Namibia and named for senior chemist Willy Reiner (1895–1965) of Tsumeb Corporation, who analyzed this mineral.[2][4]
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.
- ^ a b c Webmineral data
- ^ a b c Handbook of Mineralogy
- ^ a b c Mindat.org
- ^ a b American Mineralogist
- ^ Lutgens, Frederick, and Edward Tarbuck. Essentials of Geology. 10th. Upper Saddle River, New Jersey: Pearson Prentice Hall, 2009. 42. Print.
Content Disclaimer
Informasi ini disarikan dari Wikipedia dan disajikan kembali untuk tujuan edukasi. Konten tersedia di bawah lisensi CC BY-SA 3.0. Kami tidak bertanggung jawab atas ketidakakuratan data yang bersumber dari kontribusi publik tersebut.
- The information displayed on this website is sourced in part or in whole from Wikipedia and has been adapted for the purpose of restating it. We strive to provide accurate and relevant information, however:
- There is no guarantee of absolute accuracy. Wikipedia is an open, collaborative project that can be edited by anyone, so information is subject to change.
- It is not intended to constitute professional advice. The content displayed is for informational and educational purposes only. For important decisions (e.g., medical, legal, or financial), please consult a professional.
- Content copyright. Wikipedia is licensed under the Creative Commons Attribution-ShareAlike License (CC BY-SA). This means that content may be reused with appropriate attribution and shared under a similar license.
- Responsible use. Any risk arising from the use of information from this website is entirely the responsibility of the user.