Abstract During Late-Pleistocene,a stratigraphic sequence of alternating wind-drift sand,loess and limnetic facies developed in the northern Poyang Lake area.

• 摘 要 晚更新世期间鄱阳胡北部地区，九江、胡口、彭泽一带发育风沙-黄二湖沼相交互地层序列。