Ikranite | |
---|---|
General | |
Category | Cyclosilicate Eudialyte group |
Formula (repeating unit) | (Na,H3O)15(Ca,Mn,REE)6Fe3+2Zr3([ ],Zr)([ ],Si)Si24O66(O,OH)6Cl2−3H2O |
IMA symbol | Ikr[1] |
Strunz classification | 9.CO.10 |
Dana classification | 64.1.1.08 |
Crystal system | Trigonal |
Crystal class | Ditrigonal pyramidal (3m) H-M symbol: (3m) |
Space group | R3m |
Unit cell | a = 14.167, c = 30.081 [Å]; Z = 3 |
Identification | |
Color | Yellow to brownish yellow |
Crystal habit | Pseudo-hexagonal |
Cleavage | None |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 5 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent |
Density | 2.82 g/cm3 |
Optical properties | Uniaxial; weak anomalous biaxiality |
Other characteristics | Mildly Radioactive |
References | [2][3][4] |
Ikranite is a member of the eudialyte group, named after the Shubinov Institute of Crystallography of the Russian Academy of Sciences. It is a cyclosilicate mineral that shows trigonal symmetry with the space group R3m, and is often seen with a pseudo-hexagonal habit.[2] Ikranite appears as translucent and ranges in color from yellow to a brownish yellow. This mineral ranks a 5 on Mohs scale of mineral hardness, though it is considered brittle, exhibiting conchoidal fracture when broken.[3]
Rast
was invoked but never defined (see the help page).