Mica is a very common rock-forming mineral, widely distributed in crystalline rocks. Its general chemical formula can be expressed as:

Later, with the development of science and technology, people gradually realized that mica minerals have high insulation, high temperature resistance, strong acid and alkali resistance, and mica also began to enter building materials, fire, plastics, paper, rubber, pearlite pigments and other industries. These are mainly Muscovite and phlogopite.

Synthetic 120 mesh :large particle size, with pearl shining effect.

Lepidolite is a lithium-bearing mica, often recognized for its lavender or pink hue. It is less commonly used than the first three types, but its unique chemical composition makes it valuable for specific applications, especially in the production of lithium batteries. The lithium extracted from Lepidolite is crucial for modern technology, particularly in the growing electric vehicle market. Additionally, Lepidolite is sought after in the field of metaphysics for its believed calming properties.

Mica pigments are favored across multiple industries due to their safe and non-toxic nature, making them suitable for various applications. Some of the most common uses include:

X { Y2-3 [Z4O10] (OH)2 }

* Phlogopite-muscovite series This series comprises mica varieties that have both muscovite and phlogopite characteristics. These mixed micas are often found in metamorphic rocks and are essential for geological studies.

The common characteristics of mica group minerals are: layered silicate minerals, monoclinic crystal system, a few trigonal crystal system, the crystals are pseudo-hexagonal columnar, plate and sheet; The aggregate is scaly and foliaceous. It has a set of extremely complete cleavage, along which it is easy to peel into sheets. Therefore, the shape of mica is usually regarded as sheet.