Stone Ultra Mill

Carbon black ultrafine mill equipments is a new type machine to grind Carbon black stone into super thin Powder.
The final Powder size can be from (325 - 2500 mesh) 5micron to 47micron as per 97% passing rate.

Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate. Calcite is the primary mineral in metamorphic marble. It also occurs as a vein mineral in deposits from hot springs, and it occurs in caverns as stalactites a

Calcium fluoride ultra fine powder mill is for super-fine grinding materials with hardness less than 6 in Mohs scale and humidity less than 6 percent such as kaolin, limestone, basalt, calcite, marble, talcum, barite, gypsum, dolomite, bentonite mud, mica, pyrophyllite, sepiolite, carbon black, diatomite, graphite, alunite, fluorite, potassium feldspar, phosphorite, pigment, up to 200 kinds. The g

Mylonite ultra fine powder grinding machine is made by Clirik in 2013. Its a professionally processing calcination limestone. The granularity of the finished fineness can be adjusted bewteen 325mesh to 3000mesh. They are five types of mylonite ultra fine grinding machine: HGM80, HGM90, HGM100, HGM100A, HGM125. Working Principle of mylonite ultra fine grinding machine 1) After crushed by hammer cru

Grain Slag Ultrafine grinder Introduction At present, grain slag ultrafine grinder takes up absolute advantage in the powder pulverizing of grain slag and it has become the preferred device of grain slag powder production line. Grain slag ul

Gravel has numbers of source and names. Nature gravel is Large called conglomerate, they are a common geological feature, being formed as a result of the weathering and erosion of rocks. While natural gravel deposits are insufficient for hum

Alumina or Aluminum oxide powder can be used in many industries area, such as: aluminum industry, Precision casting, refractory products, Aluminosilicate refractory fibers, aluminous cement, and so on. Alumina/Aluminum oxide ultra fine powde

Alunite is a sulfate mineral, it occurs as veins and replacement masses in trachyte, rhyolite, and similar potassium rich volcanic rocks. It is formed by the action of sulfuric acid bearing solutions on these rocks during the oxidation and l