fluorite rock

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:

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, 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:

1. Basic Information Product Name: 90% Calcium Fluoride Fluorspar Powder / Fluorspar Lump Chemical Formula: CaF₂ CAS No.: 7789-75-5 EINECS: 232-188-7 Origin: Self-owned fluorspar mines in Mongolia Available Forms & Custom Specifications Lump: 0–5mm, 5–10mm, 10–20mm, 20–50mm adjustable Powder: 100mesh, 200mesh, 325mesh customizable fineness Appearance: Off-white crystalline solid; hard irregular lumps, free-flowing fine dry powder 2. Quality Index Standard Test Item Standard

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-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 (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

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: