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Металлургический плавиковый шпат с содержанием CaF₂ ≥97%. Сверхнизкое содержание примесей (S<0,08%, P<0,03%) обеспечивает выплавку стали и сварочных стержней высокой чистоты. Прямой источник из шахты, стабильные поставки, гибкие формы (куски/порошок) и готовность к экспорту из порта Тяньцзинь.
Металлургический плавиковый шпат с содержанием CaF₂ ≥95%. Сверхнизкое содержание примесей (S<0,08%, P<0,03%) обеспечивает выплавку стали и сварочных стержней высокой чистоты. Прямой источник из шахты, стабильные поставки, гибкие формы (куски/порошок) и готовность к экспорту из порта Тяньцзинь.
Куски монгольского плавикового шпата премиум-класса со стабильным качеством и контролируемыми примесями. Широко используется в сталеплавильном производстве, производстве ферросплавов и выплавке цветных металлов для улучшения текучести шлака и эффективности печи. Доступны индивидуальные размеры и надежные поставки по всему миру.
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: