| 全新世内蒙南缘黄旗海湖面的波动 |
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| 引用本文： | 李栓科,王涛.全新世内蒙南缘黄旗海湖面的波动[J].湖泊科学,1993,5(4):324-334. |
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| 作者姓名： | 李栓科 王涛 |
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| 作者单位： | 国家计委、中国科学院地理研究所，北京师范大学地理系 北京 100101，北京 100012铁岭市土地管理局，辽宁 112000。 |
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| 基金项目： | 国家基金委重大项目(No.9488007);中国科学院重大项目(87-45-03) |
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| 摘 要： | 黄旗海是一封闭湖泊,气候是控制其湖面变化的主要因素。地貌、沉积物、地球化学分析及历史考古资料均证实,一万年以来湖面在总体收缩下降过程巾不断地波动着。全新世初期,湖面扩张抬升,9000a B.P.前后湖面达最高(1340m),湖面面积也最大(约560km~2),其后,湖面持续地收缩下降。
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| 关 键 词： | 全新世 湖面波动 黄旗海 湖泊 |
| 收稿时间： | 1991/9/20 0:00:00 |
| 修稿时间： | 1993/5/25 0:00:00 |
Study on fluctuations of closed lake level of huangqihai lake in inner mongcolia since holocene |
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| Li Shuangke and Wang Tao.Study on fluctuations of closed lake level of huangqihai lake in inner mongcolia since holocene[J].Journal of Lake Science,1993,5(4):324-334. |
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| Authors: | Li Shuangke and Wang Tao |
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| Abstract: | Huangqihai Lake is an inland closed lake. Climatic change is a major factor to control the lake level fluctuations. The analysis on geomorphology, lacustrine sedimentology, geochemistry and historical archeology proves that the lake level has been fluctuating since 10000 a B. P. During the early Holocene, the lake level began rising and reached its maximum height at 9000a B.P. or a maximum area of the lake. Then the lake level began to fall and its surface area to be reduced successively. |
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| Keywords: | Holocene lake level fluctuation Huangqihai Lake |
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