Ganophyllite

Ganophyllite
General
CategoryMineral
Formula
(repeating unit)
(K,Na,Ca)2Mn8(Si,Al)12(O,OH)32 · 8H2O
IMA symbolGnp[1]
Strunz classification09.EG.30
Dana classification74.01.02.01
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
Space groupA2/a
Unit cell22,545.01
Identification
Formula mass1,514.2
ColorBrownish yellow to cinnamon brown
Crystal habitFoliated micaceous
CleavagePerfect on {???}
FractureBrittle
Mohs scale hardness4 - 4.5
LusterVitreous
StreakBrownish yellow
DiaphaneityTransparent to transculent
Specific gravity2.84
Density2.84
Optical propertiesBiaxial(-)
Refractive indexnα = 1.537
nβ = 1.611
nγ = 1.613
Birefringence0.076
PleochroismX = Pale yellow brown
Y = Z = Dark yellow brown
DispersionWeak
Ultraviolet fluorescenceNone
Common impuritiesFe, 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]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ Cite error: The named reference :0 was invoked but never defined (see the help page).
  3. ^ "Mineral Database - Mineralogy of Wales". National Museum Wales. Retrieved 2021-10-18.