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Found 65 Results For "
fluorspar powder
"
Espato de fluorescência de grau metalúrgico com CaF₂ ≥97%. Impurezas ultrabaixas (S≤0,08%, P≤0,03%) garantem produção de aço e hastes de soldagem de alta pureza. Fonte direta de mina, fornecimento estável, formas flexíveis (grumo/pó) e pronto para exportação do Porto de Tianjin.
Pedaços de espatoflúor de grau ácido de alta pureza com 98% e baixas impurezas (SiO₂≤1,2%, S≤0,02%). Ideal para produção de fluoroquímicos e fundição de aço. Dimensionamento personalizado, fornecimento a granel do Porto de Tianjin com preços competitivos.
Pedaços de espatoflúor de alta pureza com CaF₂ ≥90%, provenientes de depósitos da Mongólia. Apresenta qualidade estável, baixas impurezas, excelente eficiência de fluxo e vários tamanhos de partículas. Cadeia de fornecimento da mina ao porto com exportação confiável através do porto 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:
Espatoflúor metalúrgico de origem da Mongólia com 75% de CaF₂. Garante fluxo eficiente na produção de aço, impurezas controladas e fornecimento estável. Disponível em pedaços/pó com embalagens flexíveis e condições de exportação.
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:
