dolomitmárvány

Dolomitmárvány, often referred to as dolostone or dolomitic marble, is a metamorphic rock derived from the sedimentary rock dolomite. It forms when limestone or dolostone undergoes heat and pressure deep within the Earth's crust. This metamorphic process recrystallizes the original mineral grains, leading to a denser and often more visually striking material.

The composition of dolomitmárvány is primarily the mineral dolomite, a carbonate mineral with a chemical formula of calcium magnesium carbonate (CaMg(CO3)2). While pure dolomite is a significant component, dolomitmárvány can also contain varying amounts of other minerals like calcite, quartz, and various silicates, which contribute to its diverse coloration and textures.

Visually, dolomitmárvány can exhibit a wide range of colors, including whites, grays, beiges, pinks, and even greens or blues, depending on the impurities present during its formation. The texture can vary from fine-grained to coarse-grained, with the recrystallization process creating interlocking crystals. Due to its durability and aesthetic appeal, dolomitmárvány is frequently used in construction, particularly for countertops, flooring, wall cladding, and decorative architectural elements. It is also employed in sculpture and as a building material for historical monuments. Its properties make it a valuable and versatile material in both functional and artistic applications.