The burial history of the marine strata in the MidUpper Yangtze area is reconstructed by backstripping method based on the porositydepth model under complicated lithologic character. The results show that the burial history can be divided into three types，namely，early uplifthold，early upliftsubsided and late uplifthold. The regional tectonic movements controlled the burial history types which characterized by obvious zonation. The burial history types western of Qiyueshan fault belong to the late uplifthold； those between Qiyueshan fault and Huangling uplift，are the early uplifthold； those eastern of Huangling uplift，are the early upliftsubsided. The Indosinian movement resulted in a short duration of uplifting with slight erosion in the MidUpper Yangtze area and therefore significantly change of burial history was not occurred. The Yanshanian movement is the key tectonic event which influenced the burial history sorts. The differences in burial history type mainly came from the contribution of the Yanshanian movement. The Himalayan movement spread to the whole Southern China，while the lithosphere was extruded in west of Huangling uplift but extended in east of Huangling uplift. Therefore，the burial history type western of Huangling uplift is the early or late uplifthold，and those eastern Huangling uplift are the early upliftsubsided.