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Marble has a typical granular crystal structure. The particle size is generally medium and fine, sometimes coarse, and the compacted structure between calcite and dolomite particles in the rock. In the marble formed by metamorphism in some areas, the radial axis of the calcite is oriented, which makes the marble have strong light transmission. If some marble can transmit 2 cm, the transparency of individual marble. Up to 3 to 4 cm, they are excellent engraving materials. The structure of marble is mostly block-like structure, and many marbles have structures such as strips, stripes, plaques or spots of different sizes. After processing, they become decorative building materials with different colors and patterns.