Carbonate minerals are a diverse group of minerals that contain the carbonate ion (CO3^2-). They are formed through the combination of carbon dioxide and oxygen with various metallic elements, such as calcium, magnesium, and iron. The most common carbonate mineral is calcite, which is found in limestone and marble. Other examples include dolomite, malachite, and azurite.
Carbonate minerals are often formed through the deposition of calcium and other metallic ions in marine and freshwater environments. For example, limestone is formed from the accumulation and compaction of marine animal shells and skeletons over millions of years. Additionally, carbonate minerals can also precipitate from solution in caves, forming stalactites and stalagmites.
Carbonate minerals have various practical applications, including:
Understanding carbonate minerals is essential for comprehending the geology of Earth's crust and their numerous practical applications in various industries.
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