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fluorspar powder
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Espato flúor de grado metalúrgico con CaF₂ ≥97%. Las impurezas ultrabajas (S≤0,08%, P≤0,03%) garantizan una producción de acero y varillas de soldadura de alta pureza. Fuente minera directa, suministro estable, formas flexibles (en trozos/polvo) y listo para exportar desde el puerto de Tianjin.
Trozos de espato flúor de grado ácido al 98% de alta pureza con bajas impurezas (SiO₂≤1,2%, S≤0,02%). Ideal para la producción de fluoroquímicos y fundición de acero. Tamaño personalizado, suministro a granel desde el puerto de Tianjin con precios competitivos.
Trozos de espato flúor de alta pureza con CaF₂ ≥90%, procedentes de depósitos de Mongolia. Presenta una calidad estable, bajas impurezas, excelente eficiencia de fundente y múltiples tamaños de partículas. Cadena de suministro de mina a puerto con exportación confiable a través del puerto de Tianjin.
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:
Espato flúor metalúrgico de origen mongol con 75% CaF₂. Garantiza un fundente eficiente para la fabricación de acero, impurezas controladas y un suministro estable. Disponible en forma de trozos/polvo con embalaje flexible y condiciones de exportación.
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: