Jump to content

Zinnwaldite

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Vsmith (talk | contribs) at 13:28, 15 March 2009 (ref tags, rmv out of place comment). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Zinnwaldite
General
CategoryPhyllosilicate mineral
Formula
(repeating unit)
KLiFeAl(AlSi3)O10(OH,F)2
Crystal systemMonoclinic
Identification
ColorLight brown to yellowish- or greenish-white
Crystal habitMicaceous, platey scaly masses, pseudo-hexagonal phenocryst tablets
TwinningOn composition plane {001}, twin axis [310].
CleavagePerfect basal {001}
FractureUneven
TenacityLaminae flexible, elastic.
Mohs scale hardness3.5 - 4.0
LusterPearly to vitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.9 - 3.1
Optical propertiesBiaxial (-) 2V = 30°
Refractive indexnα = 1.565 - 1.625 nβ = 1.605 - 1.675 nγ = 1.605 - 1.675
Birefringence0.040 - 0.050
Pleochroismdistinct
References[1][2][3]

Zinnwaldite, KLiFeAl(AlSi3)O10(OH,F)2, is a potassium lithium iron aluminium silicate hydroxide fluoride silicate mineral in the mica group.

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.

It was first described in 1845 in Zinnwald/Cinovec on the German-Czech Republic border.

References