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Pure white Dolomite : MADOL XATICO Benelux-France Sàrl

Pure white Dolomite : MADOL

Inorganic chemistry

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Dolomite is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally CaMg(CO3)2.

The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite.

The mineral dolomite crystallizes in the trigonal-rhombohedral system. It forms white, tan, grey, or pink crystals.

Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions.

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