triphylite

mineral
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Share
Share to social media
URL
https://mainten.top/science/triphylite
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

triphylite, common phosphate mineral, lithium iron phosphate (LiFePO4), usually forming bluish or grayish, glassy masses in lithium- and phosphate-rich granite pegmatites. It forms a solid-solution series with the similar, but more brightly coloured (brown, yellow, or salmon), lithiophilite in which manganese replaces iron in the molecular structure; that is, a complete chemical variation exists in nature between the pure iron-bearing compound and the pure manganese-bearing compound. Triphylite and lithiophilite are readily weathered. When wetted, as by atmospheric moisture, the lithium ions are leached from the structure, and the iron and then manganese are oxidized to compensate for the valence (combining power) change. When subjected to hydrothermal solutions, triphylite and lithiophilite are altered to siderite, rhodochrosite, and hydrated normal phosphate minerals. For detailed physical properties, see phosphate mineral (table).