karbonatace
Karbonatace is a mineral classification that encompasses a group of naturally occurring inorganic compounds predominantly composed of carbonate ions (CO3^2-) combined with various metal cations. The most common and well-known members of this group are calcite, aragonite, and dolomite, each with distinct structural and chemical properties.
Calcite (CaCO3) is a widespread mineral found in sedimentary rocks such as limestone and marble. It crystallizes
Karbonatace minerals are significant in various geological processes, including rock formation, diagenesis, and the carbon cycle.
The formation of karbonatace minerals occurs through both biological and inorganic pathways. Biological processes involve organisms
In addition to their geological significance, karbonatace minerals have a role in environmental chemistry, especially regarding
Overall, karbonatace represents a key group within mineralogy and geology, contributing to Earth's geology, biological systems,