Mica forms in igneous, metamorphic, and sedimentary environments. Its formation usually occurs in regions where high temperatures and pressures prevail. In igneous rocks, mica can crystallize from magma as it cools. In metamorphic rocks, it often forms through the alteration of feldspar and other minerals under high heat and pressure conditions.

Natural high quality Muscovite:feel fine, soft lubrication.

In addition, lepidolite and ferrolepidolite can also be used as mineral raw materials for extracting lithium.

In short, there are significant differences between natural mica powder and synthetic mica powder in production methods, color and appearance, performance characteristics, application fields, and price and cost. Synthetic mica powder is superior to natural mica powder in terms of high temperature resistance, transparency, electrical insulation, stability and mechanical properties, while natural mica powder has more advantages in resource acquisition, cost and color. When choosing which type of mica powder to use, you can consider the high temperature resistance of the required material, electrical insulation performance, transparency and color requirements, evaluate the mechanical strength and hardness of the required material, consider chemical stability and other different application scenarios and technical requirements to make a reasonable choice.