carbonate diagenesis

Carbonate diagenesis refers to the processes that change carbonate minerals (like limestone) after they form, usually due to sediment burial, temperature changes, and chemical interactions with water. Over time, the original materials undergo alterations, such as dissolution, recrystallization, or cementation, which can affect their structure and properties. This transformation occurs in geological settings, influenced by factors like pressure and fluid composition. Understanding carbonate diagenesis is important for fields like geology and environmental science, as it impacts rock characteristics, fossil preservation, and the movement of water and resources in subsurface environments.