Fluorophlogopite is predominantly found in metamorphic rocks, particularly in those formed under high-temperature and high-pressure conditions, such as marbles and skarns. Notable locations for fluorophlogopite deposits include regions like the United States, Canada, and certain parts of Russia and Afghanistan. The mineral often coexists with other minerals such as biotite, muscovite, and garnet, contributing to its complexity and the diversity of rock formations in which it is found.

It is an indispensable and important raw material in the fields of electric heating equipment, wire and cable, aerospace and so on.

Layer upon layer of mica

It is an indispensable and important raw material in the fields of electric heating equipment, wire and cable, aerospace and so on.

Factors to Consider When Buying Mica Pigments Wholesale

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.  

X { Y2-3 [Z4O10] (OH)2 }

The mica industry is undergoing profound changes. With the help of emerging industries, the mica industry will be a large market of more than 10 billion.