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جودة مادة البناء الدرجة فلورسبار كتل CaF2 الحبيبية 80٪ الجزيئات المخصصة مصنع
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
جودة كتل فلورسبار عالية الجودة CaF2 90% تعدين الفلوريت مصنع
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
جودة 5-10 ملم فلوريت صناعية كتلة فلورسبار CaF2 85% استقرار حراري ممتاز مصنع
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
جودة الصف العادي فلورسبار CaF2 75٪ فلوريد الكالسيوم منجم نقاء عالية مصنع
Premium Mongolian Fluorite Ore (CaF₂) – High-Grade Raw Material for Global Fluorspar Supply Product Overview​ Fluorite (Calcium Fluoride, CaF₂) is a critical industrial mineral and the primary global source of fluorine. Widely used in the fluorochemical, metallurgical, glass, and ceramic industries, it is formed through magmatic-hydrothermal processes where fluoride-rich fluids precipitate and crystallize within host rock structures. Our company operates exclusive, self-owned
جودة كتل فلورسبار الصناعية نجاة عالية 97% مع استقرار كيميائي متفوق وتكوين نجاة منخفضة مصنع
فلوريت عالي النقاء (CaF₂ ≥97%) مع ثبات كيميائي فائق وشوائب منخفضة. متوفر بأحجام 5-10 مم و10-20 مم للمعالجة الصناعية الفعالة في إنتاج الفلور الكيميائي وصهره وتصنيعه.
جودة 95٪ نقاء فلوريت 30-80 مم حبيبي مقاومة درجات الحرارة العالية الفلورسبار الصناعي للمعادن والسيراميك مصنع
فلوريت نقاء 95% مع حجم حبيبي 30-80 ملم. صلابة عالية، غبار منخفض، وخصائص تدفق ممتازة للمعادن والسيراميك والأسمنت. جودة مستقرة مع تغليف الصادرات والخيارات المخصصة.
جودة فلورسبار عالية الجودة CaF2 95% فلوريت مصنع
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:
جودة فلورسبار معدني عالي الكالسيوم CaF2> 75% لصناعات الزجاج والسيراميك مصنع
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:
جودة نقاء 98% من مسحوق فلوريد الكالسيوم الفلورسبار كيميائيًا مصنع
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: