Chemistry:Kratochvílite
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Kratochvílite | |
---|---|
General | |
Category | Organic mineral |
Formula (repeating unit) | C13H10 |
Strunz classification | 10.BA.25 |
Crystal system | Orthorhombic |
Crystal class | Pyramidal (mmm) |
Space group | Orthorhombic H-M symbol: (mm2) Space group: Pnam |
Identification | |
Color | White |
Streak | White |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.578 nβ = 1.663 nγ = 1.919 |
Birefringence | δ = 0.341 |
References | [1][2][3] |
Kratochvilite is a rare organic mineral formed by combustion of coal or pyritic black shale deposits. It is a hydrocarbon with the formula of either C13H10 or (C6H4)2CH2. It is a polymorph of the aromatic hydrocarbon fluorene. It forms white, yellow to brown crystals in the orthorhombic system which occur often as a druzey encrustation. It has a specific gravity of 1.21 and a Mohs hardness of 1 to 2.
It was first described from the Nejedly mine in Bohemia, Czech Republic in 1937.[2]
References
- ↑ Kratochvilite data on Webmineral
- ↑ 2.0 2.1 Mindat.org
- ↑ "The Handbook of Mineralogy". http://www.handbookofmineralogy.com/pdfs/kratochvilite.pdf.
- ↑ 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.
Original source: https://en.wikipedia.org/wiki/Kratochvílite.
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