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Found 65 Results For "
fluorspar powder
"
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.
Куски плавикового шпата 98% высокой чистоты с низким содержанием примесей (SiO₂≤1,2%, S≤0,02%). Идеально подходит для фторхимического производства и выплавки стали. Нестандартные размеры, оптовые поставки из порта Тяньцзинь по конкурентоспособным ценам.
Куски плавикового шпата высокой чистоты с содержанием CaF₂ ≥90%, добываемые на месторождениях Монголии. Отличается стабильным качеством, низким содержанием примесей, превосходной эффективностью флюсования и частицами различных размеров. Цепочка поставок «рудник-порт» с надежным экспортом через порт Тяньцзинь.
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:
Металлургический плавиковый шпат монгольского происхождения с содержанием 75% CaF₂. Обеспечивает эффективную флюсовую обработку стали, контроль примесей и стабильную подачу. Доступен в форме кусков/порошка с гибкой упаковкой и условиями экспорта.
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:
