Eudialyte
Eudialyte, whose name derives from the Greek phrase Εὖ διάλυτος, eu dialytos, meaning "well decomposable", is a somewhat rare, nine-member-ring cyclosilicate mineral, which forms in alkaline igneous rocks, such as nepheline syenites. Its name alludes to its ready solubility in acid.
Eudialyte | |
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General | |
Category | Cyclosilicate |
Formula (repeating unit) | Na15Ca6(Fe,Mn)3Zr3SiO(O,OH,H2O)3 (Si3O9)2(Si9O27)2(OH,Cl)2 |
IMA symbol | Eud |
Strunz classification | 9.CO.10 |
Crystal system | Trigonal |
Crystal class | Hexagonal scalenohedral (3m) H-M symbol: (3 2/m) |
Space group | R3m |
Unit cell | a = 14.31, c = 30.15 [Å]; Z = 12 |
Identification | |
Color | Red, magenta, brown; also blue and yellow |
Crystal habit | Crystals short rhombohedral to long prismatic, granular, irregular masses |
Cleavage | Distinct on {0001} imperfect on {1120} |
Fracture | Uneven |
Tenacity | Brittle |
Mohs scale hardness | 5–6 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.74–3.10 |
Optical properties | Uniaxial (+/−) |
Refractive index | nω = 1.606–1.610 nε = 1.610–1.613 |
Birefringence | δ = 0.004 |
Pleochroism | Weak: O= colorless, pale yellow, pink; E= pink to colorless |
Solubility | H2SO4 |
Other characteristics | Mildly Radioactive |
References |
Eudialyte was first described in 1819 for an occurrence in nepheline syenite of the Ilimaussaq intrusive complex of southwest Greenland.
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