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[[ca:Zinnwaldita]]
[[ca:Zinnwaldita]]

Revision as of 17:15, 25 October 2010

Zinnwaldite
General
CategoryPhyllosilicate mineral
Formula
(repeating unit)
KLiFeAl(AlSi3)O10(OH,F)2
Crystal systemMonoclinic - Prismatic
Space groupMonoclinic Point Group: 2/m
Unit cella = 5.29 Å, b = 9.14 Å, c = 10.09 Å: β = 100.83°
Identification
ColorGray-brown, yellow-brown, pale violet, dark green, color zoning common
Crystal habitWell-formed short prismatic or tabular crystals, pseudohexagonal, in rosettes or fan-shaped groups; lamellar or scaly aggregates; disseminated.
TwinningOn composition plane {001}, twin axis [310]
CleavagePerfect basal {001}
FractureUneven
TenacityLaminae °exible, elastic
Mohs scale hardness3.5 - 4.0
LusterPearly to vitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.9 - 3.1
Optical propertiesBiaxial (-)
Refractive indexnα = 1.565 - 1.625 nβ = 1.605 - 1.675 nγ = 1.605 - 1.675
Birefringence0.040 - 0.050
PleochroismDistinct, X = colorless to yellow-brown; Y = gray-brown; Z = colorless to gray-brown
2V angle0 - 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