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Lepidolite Lepidolite (KLi2Al(Al,Si)3O10(F,OH)2 is a lilac-gray or rose-colored silicate minerals|phyllosilicate mineral of the mica group that is a secondary source of lithium.["Manual of Mineralogy, 20th Ed." by Cornelius Hurlbut and Cornelis Klein.] 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.[H. Nechamkin, ''The Chemistry of the Elements'', McGraw-Hill, New York, 1968.] In 1861 Robert Bunsen and Gustav Kirchhoff extracted 150 kg of lepidolite and yielded few grams of rubidium salts for analysis, and therefore discovered the new element rubidium.
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.[
Notable occurrences: Brazil; Ural Mountains, Russia; California; Tanco Pegmatite, Bernic Lake Manitoba, Canada, Madagascar.
]References
Category:Phyllosilicates
Category:Lithium minerals
category:Potassium minerals
category:Aluminium minerals
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