Zinnwaldite | |
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General | |
Category | Phyllosilicate mineral |
Formula (repeating unit) |
KLiFeAl(AlSi3)O10(OH,F)2 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Unit cell | a = 5.29, b = 9.14 c = 10.09 [Å]; β = 100.83° |
Identification | |
Color | Gray-brown, yellow-brown, pale violet, dark green, color zoning common |
Crystal habit | Well-formed short prismatic or tabular crystals, pseudohexagonal, in rosettes or fan-shaped groups; lamellar or scaly aggregates; disseminated. |
Twinning | On composition plane {001}, twin axis [310] |
Cleavage | Perfect basal {001} |
Fracture | Uneven |
Tenacity | Laminae °exible, elastic |
Mohs scale hardness | 3.5 - 4.0 |
Luster | Pearly to vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.9 - 3.1 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.565 - 1.625 nβ = 1.605 - 1.675 nγ = 1.605 - 1.675 |
Birefringence | 0.040 - 0.050 |
Pleochroism | Distinct, X = colorless to yellow-brown; Y = gray-brown; Z = colorless to gray-brown |
2V angle | 0 - 40° |
References |
Zinnwaldite, KLiFeAl(AlSi3)O10(OH,F)2, potassium lithium iron aluminium silicate hydroxide fluoride is a silicate mineral in the mica group. The IMA status is as a series between siderophyllite (KFe2Al(Al2Si2)O10(F,OH)2) and polylithionite (KLi2AlSi4O10(F,OH)2) and not considered a valid mineral species.
It was first described in 1845 in Zinnwald/Cinovec on the German-Czech Republic border.
It occurs in greisens, pegmatite, and quartz veins often associated with tin ore deposits. It is commonly associated with topaz, cassiterite, wolframite, lepidolite, spodumene, beryl, tourmaline, and fluorite.