The theoretical values of its chemical composition are K20 = 4.82% ~ 13.85%, Li20 0 = 3.87%~5.83%, A1203= 11.33% ~23.8% si02 = 46% ~60%,H2 0 = 0.65% ~3.15%. F= 1.36%~8.71%; The mixture is often Mg0, Fe0, Mn0, Ca0, Na20, Cs20, Rb2 0 and so on. The crystal is pseudohexagonal flake, but the fully developed crystal is extremely rare, often in flake or scaly form. The use of PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC magnetic field to remove iron, occasionally there are crystal clusters, the color is white or light white.
Often rose, light purple appear, occasionally also see peachy lipolite, glass luster, the cleft surface is pearl luster, hardness 2 ~ 3, the sheet has elasticity, density 2. 8 ~ 3. G /cm3. The polymetallic deposits associated with lepidolite, rubidium and cesium in tantalum-niobium ore are associated lepidolite deposits, which are also one of the main LITHIUM resources used by PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC field in mining.
Lithium nepheline: is the product of spodumene alteration, chemical composition of Li[A1s04], sometimes mixed Ca0, FE02, C1 and so on. The crystals belong to the hexagonal crystal system, the crystal shape is small, often in the form of granular aggregate and dense block production, using PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC. Color is often gray or gray with light yellow, light brown, light red, light green and other colors, sometimes also see colorless;
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