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黑龙江省哈尔滨东北郊的黄山(又名荒山),由于盛产哺乳动物化石和石器,引起第四纪工作者的普遍注意,成为我国东北第四纪地质研究的典型地区之一。但是,对黄山第四纪地层划分、时代、成因及其沉积环境的认识,至今尚未统一,1974年曾与有关单位协作,对哈尔滨黄山和肇源三站的第四纪地层进行了考察和初步总结。本文是在此基础上,对1978年于该剖面下部进行加密取样和补充分析,并结合植物残体分析和C~(14)年龄测定结果的进一步总结。
Huangshan (also known as the barren hills) in the northeastern suburb of Harbin, Heilongjiang Province, has become a typical area of Quaternary geology in northeastern China due to the abundance of mammalian fossils and stone tools, which have aroused the universal attention of Quaternary workers. However, understanding of Quaternary stratigraphy division, age, genesis and sedimentary environment of Huangshan Mountain has not been unanimously yet. In 1974, it cooperated with relevant units to study and preliminary study Quaternary strata of Huangshan and Zhaoyuan stations in Harbin to sum up. Based on this, this article is based on the analysis of the lower part of the profile in 1978, sampling and supplementary analysis, combined with plant residue analysis and C ~ (14) age determination results further summarized.