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在<地理学报>一九八一年第三期上发表的“全新世滦河三角洲相和沉积环境”一文,把滦河三角洲划分为五期亚三角洲沉积体;并根据砂体堆积形态、相的特征和冲淤动态,进而提出了各亚三角洲形成共同遵循的沉积模式。对弱潮汐河口,以河流和波浪因素为主的三角洲塑造过程具有一定的代表性。但是,该文主要内容是在1978年野外工作基础上完成的。近年来,由于实际资料和实验数据日益丰富,对某些问题有必要重新再认识。
In the article published in the third issue of Geographical Journal in 1981, the article entitled “Holocene Luanhe Delta Sedimentary Environment”, divides the Luan River Delta into five sub-delta sediments; and according to the sedimentary form of sand body, Characteristics and scouring and silting dynamics, and then put forward the formation of the common formation of sub-delta sedimentary model. For the weak tidal estuary, the process of delta shaping, mainly of rivers and waves, has certain representativeness. However, the main content of the article was completed on the basis of field work in 1978. In recent years, due to the increasingly abundant actual data and experimental data, it is necessary to re-understand some issues.