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摘要:
中国的第四纪下限研究目前虽然比较倾向于2.4~2.6 Ma, 但也存在不同的观点。在简要回顾中国第四纪研究历史的基础上, 重点介绍中国北方地区、黄河流域、西南地区、东北地区、新疆和西藏地区的第四纪下限研究历史、现状以及存在的问题, 简要介绍黄土地层剖面和南海沉积物剖面对第四纪下限研究的主要贡献, 最后以泥河湾阶的建立过程说明中国第四纪下限研究存在的不足以及应对方法。
Abstract:Lower Boundary of Quaternary period, the boundary of Quaternary and Neogene, is an important basic problem of the stratigraphic and Quaternary study's. Although currently Quaternary research in China tend to the limit of 2.4~2.6Ma, but there is still have different views. This paper briefly reviews the history of the Chinese Quaternary research, focusing on the research history, current situation and problems in Northern China, the Yellow River Basin, Southwest China, Northeast China, Xinjiang and Tibet area. The aim of paper is to give thereadera clearer understanding of China Quaternary boundary. As well as we introduced the main contribution of the South China Sea sediments and loess stratigraphic section. Finally, explained the shortcomings and the solution of lower boundary of Quaternary period in China by the process of establishing Nihewan stage.
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Key words:
- China /
- Quaternary period /
- Lower boundary /
- review
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