Chemistry:Leucophanite: Difference between revisions
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Latest revision as of 04:13, 6 February 2024
| Leucophanite | |
|---|---|
 The leucophanite on an aegirine needle (about 4–5 mm on edge) | |
| General | |
| Category | Inosilicates |
| Formula (repeating unit) | (Na,Ca) 2BeSi 2(O .OH .F) 7 |
| Strunz classification | 9.DH.05 |
| Crystal system | Orthorhombic |
| Crystal class | Disphenoidal (222) (same H-M symbol) |
| Space group | P212121 |
| Identification | |
| References | [1][2][3][4][5] |
Leucophanite is an inosilicate mineral with the chemical formula (Na,Ca)
2BeSi
2(O
.OH
.F)
7. It may contain cerium substituting in the calcium position.
It occurs in pegmatites and alkali igneous complexes as yellow, greenish or white triclinic crystals and has been found in Norway , Quebec and Russia .
It was first described from the Langesundfiord district of southern Norway in 1840. The name is from the Greek Script error: The function "transl" does not exist. for "white" and Script error: The function "transl" does not exist. for "to appear" in allusion to the common white color.
References
- ↑ Mineralienatlas
- ↑ Mindat
- ↑ Webmineral data
- ↑ Mineral data publishing – PDF
- ↑ Mineral galleries
- ↑ 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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