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品質 CaF2 ≥ 90% フロアード鉱物 フロアスパール 塊粒 10-20mm 金属類 工場
モンゴルの自営鉱山からの冶金用蛍石塊 CaF₂ 90%。厳選された原石を厳重に選別し、水分の少ない10~20mmの粒にしました。製鉄、化学原料、ガラス製造に最適なフラックスです。鉱山から天津港への直接物流により安定供給。
品質 建築用材料 グレード フルオースパール 粒状 CaF2 90% ハード 不規則 工場
1. Basic Information Product Name: Building Material Grade Fluorspar Granular Main Composition: CaF₂ ≥90% CAS No.: 7789-75-5 Appearance: Hard irregular off-white/grey crystalline granules Source: Self-owned fluorite mines in Mongolia Custom Particle Sizes: 3–8mm, 5–15mm, 10–30mm, 20–50mm customizable 2. Standard Quality Specifications Test Item Standard Index CaF₂ (Calcium Fluoride) ≥90.0% SiO₂ (Silica) ≤7.0% CaCO₃ (Calcium Carbonate) ≤2.5% Fe₂O₃ (Ferric Oxide) ≤0.20% Sulfur
品質 超高純度フルオースパール CaF2 99% カルシウムフッ化物 工場
What Is 99% Fluorspar? 99% fluorspar is the highest commercial grade of calcium fluoride (CaF₂), a pure halide mineral used as the premium raw material for fluorine-based chemistries. This ultra-high purity grade minimizes downstream purification, directly improving yield and reducing production costs for fluorochemical, metallurgical, glass, and ceramic applications. Key Functions & Applications Fluorochemical Industry: Essential for producing hydrofluoric acid (HF),
品質 高級金属工学級 フルオースパール 塊 CaF2 80% フロライト岩 工場
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:
品質 バルク原料 蛍石 CaF2 90% 10-20mm 蛍石塊 CaF₂ ≥90% 工場
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 metallurgical fluxing, ceramic manufacturing, cement production and general
品質 安定フッ素スパート CaF2 85% 10-20mm 伝統的な金属工学の陶器生産用 工場
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
品質 金属類 フロアイト塊 CaF2>70% モンゴリア鉱石 フロアスパール鉱山 工場
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:
品質 純度97%のカルシウム酸グレードの蛍石モンゴル鉱石蛍石塊 工場
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:
品質 純度70%のフッ化カルシウム蛍石塊蛍石岩安定したハイグレード 工場
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: