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Found 51 Results For "
fluorspar mineral
"
1. Basic Product Information Product Name: 92% Calcium Fluoride Fluorspar Powder, 92% Fluorspar Lump Chemical Formula: CaF₂ CAS Number: 7789-75-5 EINECS No.: 232-188-7 Source: Self-operated fluorspar mines in Mongolia Available Forms & Custom Sizes Lump: 3–8mm, 5–15mm, 10–30mm, 20–50mm,30–80mm customizable Powder: 100 mesh, 200 mesh, 325 mesh adjustable fineness Appearance: Off-white crystalline solid; hard irregular lumps, free-flowing fine powder 2. Quality Specifications
Fluorite CaF₂ 90% Purity 0–5mm Ceramic Fluorspar Lump Mineral Material Product Overview Our 90% purity Fluorite (Fluorspar) is a cost-effective industrial-grade mineral material with steady CaF₂ content reaching 90% and well-controlled harmful impurities. Processed through standardized crushing, washing and precise screening, this fluorite features uniform texture, low powder rate and stable chemical properties. It is a versatile bulk raw material, widely used in metallurgica
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, 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:
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:
