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lepidolite

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Also known as lepidolite mica series

Lepidolite is the common name for a lilac-gray or rose-colored series of minerals in the mica group. The mineralogical name for this series is the polylithionite-trilithionite series. Lepidolite has a chemical formula of . It is the most abundant lithium-bearing mineral and is a secondary source of this metal. It is also the major source of the alkali metal rubidium, which substitutes (as in all minerals) for potassium.

Key facts

Mineral.name
Lepidolite
Mineral.category
Phyllosilicate minerals
Mineral.group
Mica group, trioctahedral mica group
Mineral.series
Polylithionite-Trilithionite series
Mineral.boxbgcolor
cccccc
Mineral.image
Boromuscovite-Lepidolite-ch38a.jpg
Mineral.imagesize
260px
Mineral.IMAsymbol
Lpd
Mineral.strunz
9.EC.20
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
C2/m, Cm
Mineral.unit cell
a = 5.209(2) Å, b = 9.011(5) Å, c = 10.149(5) Å; β = 100:77(4)°; Z = 2
Mineral.color
Pink, light purple, purple, rose-red, violet-gray, yellowish, white, colorless other colors possible but are rare.
Mineral.habit
Tabular to prismatic pseudohexagonal crystals, scaly aggregates and massive
Mineral.twinning
Rare, composition plane {001}
Mineral.cleavage
{001} perfect
Mineral.fracture
Uneven

via Wikipedia infobox

Wikidata facts

Image
Lepidolita.jpeg
Show 4 more facts
Commons category
Lepidolite
Nickel-Strunz 9th edition (updated 2009)
9.EC.20
IMA Mineral Symbol
Lpd
Strunz 8th edition (series ID, updated)
VIII/E.05b
Sources (1)

via Wikidata · CC0

~6 min read

Article

4 sections
Contents
  • Description
  • Structure and composition
  • Occurrences
  • References

{{Infobox mineral | name = Lepidolite | category = Phyllosilicate minerals | group = Mica group, trioctahedral mica group | series = Polylithionite-Trilithionite series | boxwidth = | boxbgcolor = #cccccc | image = Boromuscovite-Lepidolite-ch38a.jpg | imagesize = 260px | caption = | formula = | IMAsymbol = Lpd | molweight = | strunz = 9.EC.20 | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = C2/m, Cm | unit cell = a = 5.209(2) Å, b = 9.011(5) Å, c = 10.149(5) Å; β = 100:77(4)°; Z = 2 | color = Pink, light purple, purple, rose-red, violet-gray, yellowish, white, colorless other colors possible but are rare. | habit = Tabular to prismatic pseudohexagonal crystals, scaly aggregates and massive | twinning = Rare, composition plane {001} | cleavage = {001} perfect | fracture = Uneven | mohs = 2.5–3 | luster = Vitreous to pearly | polish = | refractive = nα=1.525–1.548, nβ=1.551–1.58, nγ=1.554–1.586 | opticalprop = Biaxial (−) | birefringence = 0.0290–0.0380 | dispersion = | 2V = 0° – 58° measured | pleochroism = X = almost colorless; Y = Z = pink, pale violet | fluorescence= | absorption = | streak = White | gravity = 2.8–2.9 | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Transparent to translucent | other = | references = }}

Lepidolite is the common name for a lilac-gray or rose-colored series of minerals in the mica group. The mineralogical name for this series is the polylithionite-trilithionite series. Lepidolite has a chemical formula of . It is the most abundant lithium-bearing mineral and is a secondary source of this metal. It is also the major source of the alkali metal rubidium, which substitutes (as in all minerals) for potassium.

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