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1. Basic Product Info Product Name: 95% Fluorspar Powder, 95% Fluorspar Lump Chemical Name: Calcium Fluoride (CaF₂) CAS No.: 7789-75-5 EINECS: 232-188-7 Origin: Self-owned fluorspar mines in Mongolia Forms Available: Lump: 5–10mm, 10–30mm, 20–50mm custom sizes Powder: 100mesh / 200mesh / 325mesh adjustable fineness Appearance: Off-white crystalline solid; lumps are hard rock particles, powder is free-flowing fine dust 2. Strict Quality Standard (95% Grade) Testing Item
CaF₂ ≥90% を含む冶金グレードの蛍石。超低不純物 (S≤0.08%、P≤0.03%) により、高純度の製鋼および溶接棒の製造が保証されます。直接採掘、安定供給、柔軟な形状(塊状/粉末)、天津港からの輸出対応。
品質が安定し、不純物が管理されたプレミアムモンゴル産蛍石塊です。スラグの流動性と炉効率を向上させるために、製鋼、合金鉄の製造、非鉄金属の精錬で広く使用されています。信頼性の高いグローバル供給により、カスタマイズされたサイズをご利用いただけます。
High-Grade Mongolian Fluorspar (Fluorite, CaF₂) – Bulk Supply for Fluorochemical, Metallurgy, Glass & Ceramics Fluorite (industrially named fluorspar) is a vital halide mineral composed of calcium fluoride (CaF₂). It stands as the world’s dominant raw feedstock for fluorine-based manufacturing, widely applied in fluorochemical production, metallurgical smelting, glass melting and ceramic firing. Fluorite forms via magmatic hydrothermal mineralization: as magma cools, fluoride
Product Overview Our 85% CaF₂ Fluorite (Fluorspar) is a practical and cost-effective industrial-grade mineral material tailored for general industrial applications. With stable 85% calcium fluoride content and strictly managed impurity levels, this fluorite is processed through professional crushing, washing and precise screening. It features stable chemical properties, uniform grain shape and low dust volume, delivering consistent batch stability. Ideal for bulk industrial
Premium Acid-Grade Fluorite (CaF₂ ≥98%) – Mongolian High-Purity Fluorspar Supplier What Is Fluorite? Fluorite (calcium fluoride, CaF₂) is a natural halide mineral and the world’s leading raw material for fluorine production. It is essential for fluorochemicals, metallurgy, glass, and ceramics. Fluorite forms through magmatic-hydrothermal processes: fluoride-rich fluids from cooling magma react with calcium from surrounding rocks, crystallizing into high-purity deposits. Why