Chemistry:Inyoite
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| Inyoite | |
|---|---|
| General | |
| Category | Nesoborates |
| Formula (repeating unit) | CaB3O3(OH)5·4H2O |
| Strunz classification | 6.CA.35 |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/a |
| Unit cell | a = 10.63, b = 12.06 c = 8.4 [Å]; β = 114.03°; Z = 4 |
| Identification | |
| Colour | Colourless, white on dehydration. |
| Crystal habit | Commonly as prismatic to tabular crystals; also in cockscomb aggregates of pseudorhombohedral crystals; coarsely spherulitic or granular |
| Cleavage | Good on {001}, distinct on {010} |
| Fracture | Irregular/uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 2 |
| Vitreous|re|er}} | Vitreous |
| Specific gravity | 1.875 |
| Optical properties | Biaxial (−) |
| Refractive index | nα = 1.495 nβ = 1.505 – 1.512 nγ = 1.520 |
| Birefringence | Maximum δ = 0.025 |
| Dispersion | Weak |
| References | [1][2] |
Inyoite, named after Inyo County, California, where it was discovered in 1914, is a colourless monoclinic mineral. It turns white on dehydration. Its chemical formula is Ca(H4B3O7)(OH)·4H2O or CaB3O3(OH)5·4H2O.[2] Associated minerals include priceite, meyerhofferite, colemanite, hydroboracite, ulexite and gypsum.[1][2]
References
- ↑ 1.0 1.1 Mindat.org
- ↑ 2.0 2.1 2.2 Handbook of Mineralogy
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W.
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