Dolomite

Dolomite is a double carbonate of calcium and magnesium and it exhibits a granular structure. It has high natural whiteness and its noted for their ease of dispersion. Its use improves properties such as wheatherability, reduces shrinkage, fissure development and water absorption .
Dolomite was named for the French mineralogist Deodat de Dolomieu. The mineral dolomite is commonly found in deposits of a sedimentary rock called dolostone. There are two types of materials often called dolomite, a true chemically uniform calcium magnesium carbonate with the chemical formula CaMg(CO3)2, and a dolomitic limestone, which is just an irregular mixture of calcium and magnesium carbonates.
  D1D2
 Calcium Oxide CaO 29.4% ( + 1% ) 53.76%
 Magnesium Oxide MgO 18.4% ( + 1% ) 0.70%
 Silica SiO2  7.5% ( + 1% ) 1.64%
 Alumina Al2O3 0.24% ( + 0.05% ) 0.24%
 Ferric Oxide Fe2O3 0.48% ( + 0.05% ) 0.18%
 Loss On Ignition LOI 43.3% ( + 2% ) 43%
 Probable Composition
 Calcium Carbonate CaCO3 52.5% ( + 2% ) 96%