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Pelitic rocks, also known as pelites, are a category of sedimentary rocks composed of fine-grained particles, primarily clay or mud. These rocks are abundant, making up a significant portion of Earth's sedimentary rock column.12

Pelites include siltstone, claystone, and mudstone, with shale being a specific type of mudrock that exhibits lamination or fissility. While often formed from weathered rock material, pelites can also contain chemically precipitated cement and organic matter. Their fine grain size influences their properties, typically indicating deposition in low-energy environments where water movement is minimal.23

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