A carbonate platform is a marine geological structure characterized by significant deposits of carbonate minerals, primarily limestone and dolomite, which are formed in shallow marine environments. These platforms are typically found in tropical and subtropical regions and are associated with reef systems. Key features of carbonate platforms include: 1. **Formation**: Carbonate platforms form from the accumulation of calcium carbonate produced by organisms such as corals, shellfish, and microscopic calcareous algae.
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