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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:
85% Fluor Caf2 Grudki fluorytu z CaF₂ ≥85%. Charakteryzuje się pełnym kryształem, jednolitym rozmiarem grudek, stabilnym składem. Ekonomiczne w przypadku topników metalurgicznych, produkcji kwasu fluorowodorowego, szkła i ceramiki. Dostępne opakowania zbiorcze lub w workach typu jumbo.
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:
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:
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:
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:
Metallurgical Fluorspar Lump & Powder, CaF₂ ≥ 65% | Slag Conditioner for Smelting Product Introduction We supply metallurgical fluorspar with CaF₂ content over 65%, available in lump and powder forms. It is widely used in steel casting and non-ferrous metal smelting. The raw materials go through multiple sorting and impurity removal processes to ensure even composition and controlled harmful substances. In high-temperature smelting, it effectively adjusts slag properties and
4N High-Purity Optical Grade Fluorspar, CaF₂ ≥ 99% | Ultra-Low Impurity for High-End Optical Systems Product Introduction This is 4N high-purity optical grade fluorspar with CaF₂ content ≥ 99%, serving as a core functional substrate for manufacturing high-end optical lenses, UV/IR optical windows, precision prisms and special optical instruments. Produced from high-purity fluorspar ore through multi-stage purification, directional crystallization and precision post-treatment,
4N High-Purity Optical Grade Fluorspar (CaF₂ ≥ 99%) | Low-Arsenic for UV & IR Optics Product Introduction This is 4N high-purity optical grade fluorspar with CaF₂ content stably above 99%. It is a core raw material for UV-IR broadband optical systems, special optical lenses, high-temperature optical windows and precision prisms. Produced from carefully selected high-purity fluorspar ore through wet purification, directional crystallization, high-temperature impurity removal