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کیفیت کلوخه های فلورسپار گرید مصالح ساختمانی گرانول CaF2 80% ذرات سفارشی کارخانه
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
کیفیت کلوخه های فلورسپار درجه بالا CaF2 استخراج 90% فلوریت کارخانه
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
کیفیت 5 تا 10 میلی متری فلوریت فلور اسپار CaF2 85٪ ثبات حرارتی عالی کارخانه
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
کیفیت فلوراسپات CaF2 درجه نرمال 75٪ فلوراید کلسیم معدن خالص کارخانه
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
کیفیت تکه های فلوراسپارت صنعتی با خالصیت بالا 97 درصد با ثبات شیمیایی عالی و ترکیب کم ناخالصی کارخانه
فلوریت با خلوص بالا (CaF2 ≥97%) با پایداری شیمیایی برتر و ناخالصی کم. موجود در اندازه های 5-10 میلی متر و 10-20 میلی متر برای پردازش صنعتی کارآمد در تولید، ذوب و ساخت مواد شیمیایی فلوئور.
کیفیت 95٪ طهارت فلوریت 30-80mm دانه دار مقاومت در برابر دماهای بالا فلور اسپار صنعتی برای فلزات سازی و سرامیک کارخانه
فلوریت 95 درصد خلوص با اندازه دانه 30-80 میلی متر. سختی بالا، گرد و غبار کم و خواص شار عالی برای متالورژی، سرامیک و سیمان. کیفیت پایدار با بسته بندی صادراتی و گزینه های سفارشی.
کیفیت فلوراسپارت درجه بالا CaF2 دانه دار 95٪ فلوریت معدنی کارخانه
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:
کیفیت فلوراسپارت فلوراسیونی با کلسیم بالا CaF2>75٪ برای صنایع شیشه و سرامیک کارخانه
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:
کیفیت پودر کلوخه فلورسپار کلسیم فلوراید 98 درصد خلوص شیمیایی کارخانه
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: