Feodosiyite
| Feodosiyite | |
|---|---|
| General | |
| Category | Halide mineral |
| Formula (repeating unit) | Cu11Mg2Cl18(OH)8•16H2O |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/c |
| Unit cell | a = 12.90, b = 16.42 c = 11.96 [Å]; β = 113.69° (approximated) |
| Identification | |
| References | [1][2] |
Feodosiyite is a very rare chloride mineral, just recently approved,[1] with the formula Cu11Mg2Cl18(OH)8•16H2O. Its structure is unique.[2] Feodosiyite comes from the Tolbachik volcano, famous for many rare fumarolic minerals.[3] Chemically similar minerals, chlorides containing both copper and magnesium, include haydeeite, paratacamite-(Mg) and tondiite.[4]
References
- ^ a b "Feodosiyite: Feodosiyite mineral information and data". Mindat.org. Retrieved 2016-03-04.
- ^ a b Pekov, I.V., Zubkova, N.V., Yapaskurt, V.O., Belakovskiy, D.I., Lykova, I.S., Vigasina, M.F., Britvin, S.N., Sidorov, E.G., and Pushcharovsky, D.Y. ,2015. Feodosiyite, IMA 2015-063. CNMNC Newsletter No. 28, December 2015, 1860; Mineralogical Magazine 79, 1859–1864
- ^ "Tolbachik volcano, Kamchatka Oblast', Far-Eastern Region, Russia - Mindat.org". Mindat.org. Retrieved 2016-03-12.
- ^ "Haydeeite: Haydeeite mineral information and data". Mindat.org. Retrieved 2016-03-12.
 | This article about a specific mineral or mineraloid is a stub. You can help Wikipedia by expanding it. |