Vertisols of the Huaibei Plain have developed in parent materials deposited during the Late-Pleistocene Mid-Holocene and Late-Holocene. Palaeosolic forms are recognized as relict Vertisols and buried Vertisols.
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Citation: Liu and W., L. 1991. Formation and evolution of Vertisols in Huaibei Plain. Pedosphere. 1(1): 3-15.
