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X represents large interlayer cations, such as K+, Na+, Ca2+, Ba2+, Rb+, Cs+, etc. Y represents octahedral cations, such as Al3+, Fe2+, Mg2+, Cr3+, Ti4+, Fe3+, etc. Z is mainly Si4+ and Al3+; The ideal ratio of the additional anion (OH)- to (O)2- is 2:10, and (OH)- can be replaced by F- and Cl-. Most mica contain 4% to 5% water. Therefore, although they may be called mica, the chemical composition of different mica may be very different, for the purpose of research, we collectively refer to the minerals with this type of characteristics as mica group minerals.  

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synthetic fluorphlogopite safe_mica powder in lip gloss

Mica is a group of silicate minerals that are characterized by their layered structure. The most common types of mica used for powder include muscovite and phlogopite. These minerals are found in igneous and metamorphic rocks and are known for their excellent heat resistance and electrical insulation. Once mined, mica is processed and ground into a fine powder that can be used either in its natural state or enhanced with pigments and additives for a spectrum of colors.


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synthetic fluorphlogopite safe_mica powder in lip gloss