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Dolostones are very common in the Lower Palaeozoic of the North China Platform. They can be divided into two large groups: mud-silt-sized crystalline dolostones and saccharoid dolostones. The former can be further divided into gypsiferous and nongypsiferous mud-silt-sized crystalline dolostones and the latter into equal-sized and unequal-sized saccharoid dolostones.Gypsiferous, mud-silt-sized, crystalline...