English
Français
Deutsch
Italiano
Русский
Español
Português
Nederlandse
Ελληνικά
한국
العربية
हिन्दी
Türkçe
Indonesia
Tiếng Việt
ไทย
বাংলা
فارسی
Polski
Found 54 Results For "
fluorite lump
"
CaF₂ ≥97% 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。
CaF₂ ≥95% 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。
Mongolia Sourced High Purity Fluorite Ore | Calcium Fluoride CaF₂ Raw Mineral for Global Industrial Manufacturing Fluorite, also widely traded as fluorspar, is an essential halide mineral consisting of calcium fluoride (CaF₂). As the leading raw material for all fluorine-related industries, it underpins production in fluorochemical manufacturing, metal smelting, glass melting and ceramic fabrication. Geologically, fluorite originates from magmatic hydrothermal mineralization.
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
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
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:
