Niedermayrite
Niedermayrite | |
---|---|
General | |
Category | Sulfate mineral |
Formula (repeating unit) | Cu4Cd(SO4)2(OH)6·4H2O |
Strunz classification | 7.DD.30 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/m |
Unit cell | a = 5.543(1), b = 21.995(4) c = 6.079(1) [Å]; β = 92.04(3)°; Z = 2 |
Identification | |
Color | Bluish green |
Crystal habit | Platy euhedral crystals and as green crusts |
Cleavage | Perfect on {010} |
Tenacity | Brittle |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent |
Specific gravity | 3.292 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.599 - 1.619 nβ = 1.642 nγ = 1.661 |
Birefringence | δ = 0.062 |
2V angle | Measured: 84° |
References | [1][2] |
Niedermayrite is a rare hydrated copper cadmium sulfate hydroxide mineral with formula: Cu4Cd(SO4)2(OH)6·4H2O. It crystallizes in the monoclinic system and occurs as encrustations and well formed vitreous blue-green prismatic crystals. It has a specific gravity of 3.36.
Niedermayrite was named for Gerhard Niedermayr (born 1941), an Austrian mineralogist. It was first described in 1998 from a mine in the Lavrion District, Attica, Greece. It is also reported from the Ophir District, Tooele County, Utah.[1] The environment is in brecciated marble. The cadmium dominant analogue of campigliaite.
References[]
Categories:
- Cadmium minerals
- Copper(II) minerals
- Sulfate minerals
- Monoclinic minerals
- Minerals in space group 11
- Sulfate mineral stubs