| 长江三角洲南部下蜀黄土与硬粘土层关系初探 |
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| 引用本文： | 张瑞虎,郭平,肖霞云.长江三角洲南部下蜀黄土与硬粘土层关系初探[J].鲁东大学学报,2002,18(2):113-117. |
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| 作者姓名： | 张瑞虎 郭平 肖霞云 |
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| 作者单位： | 南京师范大学地理科学学院 江苏南京210097
(张瑞虎，郭平)，南京师范大学地理科学学院 江苏南京210097(肖霞云) |
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| 摘 要： | 从气候变化和地形影响两个角度 ,对长江三角洲南部晚更新世地层中西部丘陵区的下蜀黄土与东部平原区的硬粘土层进行了初步探讨 ,认为二者的物质来源都是末次冰期盛冰期由风力搬运堆积而形成的。
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| 关 键 词： | 长江三角洲 下蜀黄土 硬粘土 |
| 文章编号： | 1004-4930(2002)02-0113-05 |
| 修稿时间： | 2002年2月2日 |
A preliminary study on the relations between Xiashu Loess and hard clay in the Yangtze River Delta |
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| ZHANG Rui hu,GUO Ping,XIAO Xia yun.A preliminary study on the relations between Xiashu Loess and hard clay in the Yangtze River Delta[J].Ludong University Journal (Natural Science Edition),2002,18(2):113-117. |
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| Authors: | ZHANG Rui hu GUO Ping XIAO Xia yun |
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| Abstract: | According to the analysis of climatic changes and terrain influence,the relations between Xiashu Loess in the western hills and the hard clay in the eastern plain, which both exist in the layers of Late Pleistocene in the southern Yangtze River Delta are discussed.The results show that Xiashu Loess and the hard clay both stem from the accumulations carried by wind in Pleniglacial of the Last Glaciation. |
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| Keywords: | Yangtze River Delta Xiashu Loess hard clay |
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