Introduction to the structure and morphology of zircon
Zircon is a silicate mineral, which can be divided into two types: high type and low type according to its physical properties and chemical composition. Completely crystallized crystals are mostly "high"; those with extremely poor or no crystals are "low". Due to the radioactive elements, the internal structure of zircon is damaged. According to the internal structure characteristics, it is divided into three types: high-type zircon, medium-type zircon and low-type zircon. But in terms of gem value, high-type zircon is more valuable.

The crystals of zircon belong to tetragonal system, a0 = 0.662nm, c0 = 0.602nm; Z = 4. In the structure, Zr and Si are arranged along the c axis to form a tetrahedral unit cell. The crystal structure can be considered as a combination of [SiO4] tetrahedron and [ZrO8] triangular dodecahedron. [ZrO8] Triangular dodecahedrons are closely connected in a co-edge manner in the b-axis direction.
Zircon is a gem with special properties. It has a high refractive index and strong dispersion. Colorless or light blue varieties have a strong fire phenomenon like diamonds after processing. Because it is similar in appearance to diamonds, it is known as a gem comparable to diamonds.
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