Chemistry:Aliettite
| Aliettite | |
|---|---|
 Aliettite | |
| General | |
| Category | Phyllosilicates |
| Strunz classification | 9.EC.60 |
| Crystal system | Hexagonal Unknown space group |
| Unit cell | a = 5.216, c = 24.6 [Å]; Z = 1 |
| Identification | |
| Color | Colorless, pale yellow or green. |
| Crystal habit | Platy |
| Mohs scale hardness | 1–2 |
| |re|er}} | Earthy (dull) |
| Streak | White |
| Diaphaneity | Translucent |
| Refractive index | 1.558–1.567 |
| References | [1][2][3][4] |
Aliettite is a complex phyllosilicate mineral of the smectite group with a formula of (Ca0.2Mg6(Si,Al)8O20(OH)4·4H2O)[1] or [Mg
3Si
4O
10(OH)
2](Ca
0.5,Na)
0.33(Al,Mg,Fe2+)
2
-
3(Si,Al)
4O
10(OH)
2·n(H
2O).[2][3]
It is a soft, colorless to pale yellow or green earthy mineral which crystallizes in the monoclinic system as minute tabular to platy crystals.[1]
It was first described in 1968 for an occurrence in Monte Chiaro, Albareto, Parma Province, Emilia-Romagna, Italy and named for the Italian mineralogist Andrea Alietti (born 1923).[1]
It occurs in serpentinized ophiolites and their residual soil. It also occurs in altered dolomite. Associated minerals include talc, chlorite, serpentine and calcite.[3] In addition to the type locality in Italy it has been reported from Kinshasa, Katanga;[3] the Chelyabinsk Oblast of the southern Urals and the Turii alkaline Massif of the Kola Peninsula in Russia ; the Zirabulak Mountains of Uzbekistan; and the Goldstrike Mine of Eureka County, Nevada, US.[1]
References
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