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本文提出海岸风沙沉积和海岸风尘沉积是晚更新世期间，由东北季风风系控制的风沙流活动所成。每一期风沙流活动的时限不恒定，其盛行风向前缘随着风力衰减而产生风尘沉积，形成海岸风沙—海岸风尘沉积匹配带。中国海岸带自北而南可划分出四个海岸风沙—海岸风尘沉积匹配区。海岸风沙－海岸风尘沉积均具有多发、高频变化特征，与其中交互更叠的土壤层、冲－洪积层、侵蚀间断面等一起，可成为晚更新世期间气候－环境判别的标志。
This paper proposes that the deposition of coastal wind-blown sand and coastal dust deposition are caused by wind-blown sand activities controlled by the northeast monsoon wind during the late Pleistocene. The duration of each phase of sand flow is not constant. The leading edge of its prevailing wind direction produces dust deposition as the wind decays, forming a coastal sand-dust deposition matching belt. China’s coastal zone can be divided into four coastal sandstorms-coastal dust deposition matching areas from north to south. Coastal winds-coastal dust deposits are characterized by multiple and high-frequency variations. Together with the more overlapping layers of soil, flood-flood accumulation and erosional discontinuities, these can be the hallmarks of climate-environment discrimination during Late Pleistocene.