Lepidolite
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| Lepidolite | |
|---|---|
 Crystal of lepidolite, Brazil |
|
| General | |
| Category | Silicate mineral |
| Chemical formula | KLi2Al(Al,Si)3O10(F,OH)2 |
| Identification | |
| Color | Pink, purple, rose-red, violet-gray, yellowish, white, colorless |
| Crystal habit | Tabular to prismatic pseudohexagonal crystals, scaly aggregates and massive |
| Crystal system | Monoclinic |
| Twinning | Rare, composition plane |
| Cleavage | [001] Perfect |
| Fracture | Uneven |
| Mohs scale hardness | 2.5–3 |
| Luster | Vitreous to pearly |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 2.8–2.9 |
| Optical properties | Biaxial (-) |
| Refractive index | a=1.525–1.548, b=1.551–1.58, g=1.554–1.586 |
| Birefringence | 0.0290–0.0380 |
| References | [1][2] |
Lepidolite (KLi2Al(Al,Si)3O10(F,OH)2 is a lilac-gray or rose-colored phyllosilicate mineral of the mica group that is a secondary source of lithium.[3] It is associated with other lithium-bearing minerals like spodumene in pegmatite bodies. It is one of the major sources of the rare alkali metals rubidium and caesium.[4] In 1861 Robert Bunsen and Gustav Kirchhoff extracted 150 kg of lepidolite and yielded a few grams of rubidium salts for analysis, and therefore discovered the new element rubidium.[5]
It occurs in granite pegmatites, in some high-temperature quartz veins, greisens, and granites. Associated minerals include quartz, feldspar, spodumene, amblygonite, tourmaline, columbite, cassiterite, topaz, and beryl.[1]
Notable occurrences: Brazil; Ural Mountains, Russia; California; Tanco Pegmatite, Bernic Lake Manitoba, Canada, Madagascar.
References
- ^ a b http://rruff.geo.arizona.edu/doclib/hom/lepidolite.pdf Handbook of Mineralogy
- ^ http://webmineral.com/data/Lepidolite.shtml Webmineral
- ^ Hurlbut, Cornelius S.; Klein, Cornelis (1985), Manual of Mineralogy, Wiley, (20th ed.) ISBN 0-471-80580-7
- ^ H. Nechamkin, The Chemistry of the Elements, McGraw-Hill, New York, 1968.
- ^ G. Kirchhoff, R. Bunsen (1861). "Chemische Analyse durch Spectralbeobachtungen". Annalen der Physik und Chemie 189 (7): 337–381. doi:10.1002/andp.18611890702.
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