Ganophyllite | |
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General | |
Category | Mineral |
Formula (repeating unit) | (K,Na,Ca)2Mn8(Si,Al)12(O,OH)32 · 8H2O |
IMA symbol | Gnp[1] |
Strunz classification | 09.EG.30 |
Dana classification | 74.01.02.01 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) |
Space group | A2/a |
Unit cell | 22,545.01 |
Identification | |
Formula mass | 1,514.2 |
Color | Brownish yellow to cinnamon brown |
Crystal habit | Foliated micaceous |
Cleavage | Perfect on {???} |
Fracture | Brittle |
Mohs scale hardness | 4 - 4.5 |
Luster | Vitreous |
Streak | Brownish yellow |
Diaphaneity | Transparent to transculent |
Specific gravity | 2.84 |
Density | 2.84 |
Optical properties | Biaxial(-) |
Refractive index | nα = 1.537 nβ = 1.611 nγ = 1.613 |
Birefringence | 0.076 |
Pleochroism | X = Pale yellow brown Y = Z = Dark yellow brown |
Dispersion | Weak |
Ultraviolet fluorescence | None |
Common impurities | Fe, Zn, Pb, Ca, Ba |
Other characteristics | Radioactive 3.87% (K) |
Ganophyllite is a phyllosilicate mineral. It was named by Axel Hamberg in 1890 from the Greek words for leaf (φύλλον) and luster (γανωμα); the latter one was chosen due to the lustrous cleavages. The mineral was approved by the IMA in 1959, and it is a grandfathered mineral, meaning its name is still believed to refer to an existing species until this day.[2] Tamaite is the calcium analogue, while eggletonite is the natrium analogue of said mineral.[3]
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