| 长江谷地更新世气候 |
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| 引用本文： | 邓玲玲.长江谷地更新世气候[J].贵州师范大学学报(自然科学版),2006,24(3):29-32. |
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| 作者姓名： | 邓玲玲 |
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| 作者单位： | 贵州师范大学,地理与生物科学学院,贵州,贵阳,550001 |
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| 基金项目： | 致谢：在何才华教授的悉心指导下完成. |
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| 摘 要： | 更新世中国东部盛行季风,长江谷地产生冰川,庐山冰川发育、更新世亚洲东部雪线降低,鄱阳湖畔有发育完美的羊背石及冰溜面,终碛及冰水沉积物。有3次冰川期:庐山鄱阳冰川期、大姑冰川期、庐山冰川期
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| 关 键 词： | 更新世 亚洲东部雪线降低 庐山冰川 |
| 文章编号： | 1004-5570（2006）03-0029-04 |
| 收稿时间： | 2006-01-16 |
| 修稿时间： | 2006-01-16 |
The Pleistocene climate of Changjiang valley |
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| DENG Ling-ling.The Pleistocene climate of Changjiang valley[J].Journal of Guizhou Normal University(Natural Sciences),2006,24(3):29-32. |
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| Authors: | DENG Ling-ling |
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| Institution: | School of Geogrophy and Biology, Guizhou Normal University, Guiyang, Cuizhou 550001, China |
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| Abstract: | When the monsoon was prevail in eastern China in Pleistocene,glaciers were produced in Chang jiang valley,The Lushan Glacier was developed and the snow line was descended in Eastern Asia.Perfect roche moutonnee,glacial striation,terminal moraine and glaciofluvial deposit were developed on Poyang Lake.There were three ice ages:Lushan-Poyang ice age,Dagu ice age and Lushan ice age. |
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| Keywords: | Pleistocene descended snow line in Eastern Asia the Lushan Glacier |
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