Schröckingerite
| Schröckingerite | |
|---|---|
 | |
| General | |
| Category | Carbonate minerals |
| Formula (repeating unit) | NaCa3(UO2)[F|(CO3)3(SO4)]·10(H2O)[1] |
| Strunz classification | 05.EG.05 |
Schröckingerite is a radioactive yellow uranium-containing carbonate mineral, hydrated sodium calcium uranyl sulfate carbonate fluoride.[2][3][4] Schröckingerite crystallizes in the orthorhombic system, occurring as globular clusters, and fluoresces yellow-green under ultraviolet light.
Schröckingerite was first described in 1783 from an occurrence in Jáchymov, Bohemia, Czech Republic, and named for its discoverer, Julius Freiherr Schrockinger von Neudenberg (1814–1882).[2][4]
References
- ↑ Sometimes presented as: (NaCa3(UO2)(CO3)3(SO4)F·10(H2O)
- ↑ 2.0 2.1 http://www.webmineral.com/data/Schrockingerite.shtml Webmineral
- ↑ http://www.mindat.org/min-3584.html Mindat
- ↑ 4.0 4.1 "Schrockingerite". OpticalMineralogy.com. Retrieved 15 December 2011.