SEA-LEVEL CHANGE AND DEPOSITS IN THE LOWER REACH (FROM HUKOU TO ZHENJIANG) OF CHANGJIANG RIVER IN HOLQCENE
全新世海面变化与长江下游近河口段的沉积作用

The flood land deposits formed in Holocene was around 30-40m in thickness in the lower reach (from Hukou to Zhenjiang) of Changjiang valley, exceeding enormously "the normal thickness" of the flood land deposits formed generally in other valleys, which was related to the constant rise of the flood stage in that period. The latter was resulted directly of indirectly from sea level rise in Holocene.