Supply Yanshan stone Zhongshan stone Shoushan stone

There are many types of stones produced in Yanshan, including typical karst stalactite formations, limestone layers, quartzite phylloshale, slate sea erosion sedimentary rocks, etc. For example, moiré stone tiles, well stones, yellow wax stones, tens of thousands of stones, foggy marble, etc. are all collectively referred to as Yanshan stones. They have greatly opened up the road to stone appreciation in Beijing. Various types of ornamental stones are commonly seen, including gray, green, brown, Chu red, blue, pure white, blue, gray, yellow, etc. The texture is lifelike, full of changes, simple texture, solemn luster, and extremely rich in shape.

Zhongshan stone is produced in the Zhongshan area of Hukou County, Jiangxi Province. Zhongshan stones come in various shapes and colors, most of which are purple-red and belong to the andesite type. Due to different textures and structures, it can produce different crisp and pleasant sounds, and can be divided into musical scales, which is relatively unique. Shizhong Mountain is located in Shuangzhong Town, Hukou County. The one to the south of the town is called Shang Shizhong Mountain, and the one to the north of the town is called Lower Shizhong Mountain. Their relative heights are only a few meters. Zhongshan stones are scattered sparsely on Shizhong Mountain, so they are extremely precious.
Shoushan stone is a volcanic hydrothermal metasomatic < (filling < ) type deposit. It dates back to about < hundreds of millions of years in the Jurassic. Due to volcanic eruptions, pyroclastic rocks were formed, and then in the gaps between volcanic eruptions or after the eruption ended. , accompanied by a large amount of acidic gas hydrothermal activity, metasomatically decomposes feldspathic minerals in the surrounding rocks, leaching out impurities such as < < < < <, while remaining more stable elements such as < < and other elements can recrystallize and form minerals, or The << mass sol dissolved out of the rock precipitates and crystallizes along the cracks in the surrounding rock to form minerals.