Serpentine is a general term for a type of magnesium rich silicate mineral that contains water, such as serpentine, serpentine, and fibrous serpentine. Their color is usually green, but there are also shades of green, light gray, white, or yellow. Serpentine stones are named because they are often green and green in color, resembling snake skin. Serpentine rocks are often distributed at the top of larger ultrabasic rocks in a cap like or edge like manner, and sometimes in a vein like or irregular shape. Smaller rock masses often completely erode into serpentinite. The minerals related to serpentinite include chromium, nickel, cobalt, platinum, asbestos, talc, magnesite, etc. Serpentine rock is also a good fertilizer ingredient.

Marble originally refers to white limestone with black patterns produced in Dali, Yunnan Province. Its cross-section can form a natural ink landscape painting. In ancient times, marble with formed patterns was often selected to make painting screens or inlaid paintings. Later on, the name marble gradually evolved to refer to limestone with various colors and patterns used as building decoration materials. White marble is generally called White Marble, but it is also called marble for the white marble used to make statues in the West. There is a saying about the name of marble - in the past, Dali in China had the best quality marble. Named after it.

Green mud amphibolite schist is a metamorphic rock formed by regional metamorphism, including basalt, tuff, gabbro, diabase, and other rocks. It represents a metamorphic environment of about 500-600 degrees Celsius and a pressure of less than ten kilobars. Its main minerals are chlorite and amphibole, with amphibole content greater than 40%. It may also contain small amounts of minerals such as plagioclase, epidote, biotite, pyrite, etc. Green mudstone, dark green in color, carved into small pieces with a small knife to appear light green, extremely fine and scaly. Hornstone schist is a common rock in orogenic belts and ancient metamorphic terrains, and is a characteristic feature of regional metamorphic amphibolite facies.