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Pure white Dolomite : MADOL XATICO Benelux-France Sàrl

Pure white Dolomite : MADOL

Inorganic chemistry

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Dolomite, which originally comes from southern Europe, is extremely white. 
 
Dolomite is a double carbonate with an alternative structural arrangement of calcium and magnesium ions involved in the formation of white, brown, grey or pink crystals, and is also considered an anhydrous type of mineral.
 
Thanks to a latest generation production plant, the MADOL range offers fine grades with a perfectly controlled grain size distribution. 
 
Depending on the grade, the average cut (D50) varies from 2 µm to 10 µm.
 
MADOL 10 -D50 = 2µm
MADOL 100 - D50 = 10µm
 

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