Dolomiitin

Dolomiitin, commonly known as dolomite, is a carbonate mineral with the chemical formula CaMg(CO3)2. It crystallizes in the trigonal-rhombohedral system and typically forms pale-colored, transparent to translucent rhombohedra, though it is often found in massive or granular rock. Dolomite occurs in a range of colors from white and gray to pink or brown due to impurities. The mineral has a Mohs hardness of about 3.5–4 and shows rhombohedral cleavage. It may exhibit a weak reaction to cold dilute hydrochloric acid, particularly when powdered or in powdered samples.

Formation and occurrence:

Dolomite forms mainly through diagenetic alteration of limestone in the presence of magnesium-rich fluids, a process known as dolomitization. It can also develop in hydrothermal environments. When the carbonate mineral dolomite dominates a rock, the resulting sedimentary rock is called dolostone. Dolostone is widespread in sedimentary basins and is an important component of many carbonate platforms and ancient rock sequences. Economically important dolostone deposits are found in various regions around the world.

Etymology and uses:

The mineral is named after the French geologist Déodat Gratet de Dolomieu, who described it in the 18th century. Dolomite and dolostone have several practical uses: they are quarried as building and decorative stone, used as an aggregate, and processed to produce lime for industrial and agricultural applications. Dolomite lime, in particular, is employed to neutralize soil acidity and supply magnesium to soils and plants. In petroleum geology, dolostone can serve as a reservoir rock in some sedimentary basins.