Lepidolite crystal can only originate in geochemical conditions where the rich composition of lithium minerals is accessible for mineral formation. Lepidolite crystal is an uncommon mineral as these geochemical conditions once in a while happen.
Greisens, Pegmatites, and Aqueous quartz veins are rock pieces of late-stage basalt crystallization. They are the pieces where much of the globe’s lithium minerals are discovered. In these rocks, Lepidolite crystal formed as dispersed particles, a total of high-quality grains, “books” of level sheets, and a total of bent sheets. Most stores of lithium minerals originated by molten processes are tiny pod-shaped repositories of hundred or thousand tons where hand mining and hand division are needed.
Noteworthy occurrences of Lepidolite crystals have been discovered in Minas Gerais (Brazil), Honshu (Japan), Manitoba (Canada), the Ural Mountains, (Russia), Madagascar, Maine, Skuleboda (Sweden), California, United States, New Mexico, & Western Australia.
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