Zinnwaldite
| Zinnwaldite | |
|---|---|
 | |
| General | |
| Category | Phyllosilicate mineral |
| Formula (repeating unit) | KLiFeAl(AlSi3)O10(OH,F)2 |
| Crystal system | Monoclinic - Prismatic |
| Space group | Monoclinic Point Group: 2/m |
| Unit cell | a = 5.29 Å, b = 9.14 Å, 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 | [1]Cite error: The <ref> tag has too many names (see the help page).[2] |
Zinnwaldite, KLiFeAl(AlSi3)O10(OH,F)2, is a potassium lithium iron aluminium silicate hydroxide fluoride silicate mineral in the mica group.
Name and discovery
It was first described in 1845 in Zinnwald/Cinovec on the German-Czech Republic border.[2]
Occurrence
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.[1]
References
- ^ a b http://rruff.geo.arizona.edu/doclib/hom/zinnwaldite.pdf Handbook of Mineralogy
- ^ a b http://mindat.org/min-4419.html Mindat
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