Is iron and calcium and magnesium replaced?
The structure of dolomite is basically composed of calcium carbonate and unequal amounts of iron, magnesium and manganese. Dolomites are mostly fluorescent. A secondary ore formed by the presence of limestone and dolomite in the presence of magnesium containing solutions.
A carbonate mineral of calcium and iron. Pure dolomite has not been found; in natural species, a lot of magnesium or manganese displaces iron. Dolomite is a member of the chemical replacement series of dolomite (dolomite), which completely replaces iron in the crystalline structure of dolomite. The physical and chemical properties of dolomite are the same as those of dolomite. The chemical formula is Ca (Fe, Mg) (CO3) 2.
A carbonate mineral of calcium and iron. Pure dolomite has not been found; in natural species, a lot of magnesium or manganese displaces iron. Dolomite is a member of the chemical replacement series of dolomite (dolomite), which completely replaces iron in the crystalline structure of dolomite. The physical and chemical properties of dolomite are the same as those of dolomite. The chemical formula is Ca (Fe, Mg) (CO3) 2.
