Flussspat CaF2 98 %
Fluorite, chemically calcium fluoride (CaF₂), is a typical halide mineral and the primary global feedstock for fluorine supply across fluorochemical, metallurgical, glass and ceramic industries. It forms endogenously from magmatic hydrothermal activity. During magma cooling, magma-separated hydrothermal fluids are rich in fluoride constituents. As these fluids migrate upward through rock fractures, gradual drops in temperature and pressure trigger a chemical reaction:
Hochwertiger Flussspat in mongolischer Säurequalität mit CaF₂ ≥98 %, geringen Verunreinigungen und stabiler Qualität. Ideal für die Herstellung von Flusssäure, Fluorchemikalien, Aluminiumfluorid und Lithiumbatteriematerialien.