English
Français
Italiano
Русский
Español
Português
Nederlandse
Ελληνικά
日本語
한국
Polski
فارسی
বাংলা
ไทย
Tiếng Việt
العربية
हिन्दी
Türkçe
Indonesia
Found 41 Results For "
fluorspar caf2
"
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:
Product Overview Our 90% purity Fluorite (Fluorspar) is a cost-effective industrial-grade mineral material with steady CaF₂ content reaching 90% and well-controlled harmful impurities. Processed through standardized crushing, washing and precise screening, this fluorite features uniform texture, low powder rate and stable chemical properties. It is a versatile bulk raw material, widely used in metallurgical fluxing, ceramic manufacturing, cement production and general
Metallurgischer Flussspat mit CaF₂ ≥85 %, geringe Verunreinigungen. Verbessert die Effizienz der Stahlherstellung und die Leistung des Schweißstabs. Direkte Minenquelle, stabile Versorgung, flexible Formen und Verpackungen. Exportbereit aus Tianjin.
4N Optical Grade Fluorspar | CaF₂ ≥ 99% for Precision Optics Product Introduction Our high-purity optical grade fluorspar has CaF₂ content ≥ 99% (4N). It is a core raw material for manufacturing high-end optical lenses, prisms and optical instruments. With extremely low impurity levels, it features excellent light transmittance, low dispersion and thermal stability, effectively eliminating chromatic aberration and improving imaging clarity. Core Advantages Ultra-High 4N
Fluorite (Calcium Fluoride / CaF₂) – Core Fluorine Raw Mineral Fluorite, also widely traded as fluorspar, is a vital halide mineral and the world’s dominant raw material for all fluorine-based manufacturing. Key downstream industries relying on high-quality fluorspar include fluorochemical production, steel metallurgy, glass smelting, enamel and ceramic manufacturing. Fluorite deposits form via magmatic hydrothermal geological processes. Hydrothermal fluids rich in fluorides
1. Basic Product Info Product Name: 95% Fluorspar Powder, 95% Fluorspar Lump Chemical Name: Calcium Fluoride (CaF₂) CAS No.: 7789-75-5 EINECS: 232-188-7 Origin: Self-owned fluorspar mines in Mongolia Forms Available: Lump: 5–10mm, 10–30mm, 20–50mm custom sizes Powder: 100mesh / 200mesh / 325mesh adjustable fineness Appearance: Off-white crystalline solid; lumps are hard rock particles, powder is free-flowing fine dust 2. Strict Quality Standard (95% Grade) Testing Item
High-Quality Mongolia Fluorspar (Fluorite) Bulk Supply | CaF₂ Ore & Powder Fluorspar (chemically known as Calcium Fluoride, $CaF_2$) is the primary global feedstock for the fluorine supply chain. It is widely used across the fluorochemical, metallurgical (steelmaking & aluminum smelting), glass, and ceramic industries. Our enterprise owns and operates exclusive, premium fluorite mining bases in Mongolia. We deliver stable, large-scale, and high-purity fluorspar products
Fluorite, also known as fluorite, is the crystal of calcium fluoride with the chemical formula CaF2. As an important mineral raw material for modern industry, fluorite is a precious non-renewable scarce resource and mainly used in strategic emerging industries such as new energy, new materials, as well as some traditional fields like metallurgical, chemical, construction materials, optical industry etc. Mongolia ore bodies feature naturally high calcium fluoride content with
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:
