Mineralogy
Diagenesis refers to the physical and chemical processes that occur in sediments after their deposition and during their lithification, transforming them into sedimentary rock. This process can significantly alter the mineral composition, texture, and structure of the original sediment, influencing the properties of carbonate minerals, hydroxides, and even gemstones. Diagenesis plays a critical role in shaping the geological history and economic value of these materials.
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