The Terrain and Climatic Change of Jianghan Plain since Holocene
Abstract: Based on the borehole of Jianghan Plain as the research object, the date of 10 boreholes located in the East-West of Jianghan Plain were collected. These data were published by previous studies. Stratigraphic map from west to east of the Jianghan Plain is drawn out through comprehensive analysis of these drilling data. Through the analysis of drilling data, the terrain and climatic change since Holocene have been reconstructed. The research result shows that terrain and climatic changes of Jianghan Plain can be divided into three stages as follows: in 10 - 7 ka BP, most of the regions were relatively flat. Tancaidou village in Qinshi country and Miancheng area were relatively low. This period were mainly formed by river cutting action; during 7 - 3 ka BP because of the Yangtze river and Hanjiang river flood deposit development, the sediment carried by flood accumulate rapidly in relatively low area of Tancaidou village in Qinshi country and Miancheng area; ~3 ka BP many low-lying areas and some deep grooves have basically been filled. Then Jianghan Plain terrain influenced by human is growing.
文章引用: 陈思思 , 王熊飞 (2014) 全新世以来江汉平原地形及其环境变化探讨。 地理科学研究， 3， 39-45. doi: 10.12677/GSER.2014.34005
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