Lepidolite

Lepidolite is a lilac-gray or rose-colored member of the mica group of minerals with chemical formula K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2. It is the most abundant lithium-bearing mineral and is a secondary source of this metal. It is the major source of the alkali metal rubidium.

Lepidolite
General
CategoryPhyllosilicate
Formula
(repeating unit)
K(Li,Al)3(Al,Si,Rb)4O10(F,OH)2
IMA symbolLpd
Strunz classification9.EC.20
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/m, Cm
Unit cella = 5.209(2) Å, b = 9.011(5) Å,
c = 10.149(5) Å;
β = 100:77(4)°; Z = 2
Identification
ColorPink, light purple, purple, rose-red, violet-gray, yellowish, white, colorless other colors possible but are rare.
Crystal habitTabular to prismatic pseudohexagonal crystals, scaly aggregates and massive
TwinningRare, composition plane {001}
Cleavage{001} perfect
FractureUneven
Mohs scale hardness2.5–3
LusterVitreous to pearly
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.8–2.9
Optical propertiesBiaxial (−)
Refractive indexnα=1.525–1.548, nβ=1.551–1.58, nγ=1.554–1.586
Birefringence0.0290–0.0380
PleochroismX = almost colorless; Y = Z = pink, pale violet
2V angle0° – 58° measured
References

Lepidolite is found with other lithium-bearing minerals, such as spodumene, in pegmatite bodies. It has also been found in high-temperature quartz veins, greisens and granite.

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