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fluorspar lumps
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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:
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:
1. Basic Product Information Product Name: Building Material Grade Fluorspar Granular Chemical Composition: CaF₂ ≥80% CAS No.: 7789-75-5 Appearance: Irregular off-white / light grey hard mineral granules Origin: Self-owned fluorite mines in Mongolia Custom Particle Size: 5–10mm, 10–30mm, 30–70mm adjustable per client demand 2. Quality Index (Standard Specification) Inspection Item Standard Value Calcium Fluoride (CaF₂) ≥80.0% Silica (SiO₂) ≤12.0% Calcium Carbonate (CaCO₃) ≤1
Fluorite (Calcium Fluoride – CaF₂) – High-Grade Mongolian Fluorite Ore Supplier Fluorite (calcium fluoride, CaF₂) is a key halide mineral and the world’s primary source of fluorine for the fluorochemical, metallurgical, glass, and ceramic industries. It forms naturally from magmatic hydrothermal activity: as magma cools, fluoride-rich hydrothermal fluids migrate upward through rock fractures, reacting with calcium ions from wall rocks to precipitate and crystallize into
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 ≥65% CaF₂ | Lump & Powder for Steelmaking & Foundry 2. Product Introduction Metallurgical grade fluorspar is a fundamental industrial flux material, available in both lump ore and fine powder forms. It is produced from carefully selected fluorspar ore, processed through crushing, screening, and optional grinding to meet the standard requirement of CaF₂ ≥65%. The product is designed to perform reliably in high-temperature metallurgical environments,