| 南黄海西部“阿尼努德振动”现象的初步研究 |
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| 引用本文： | 于洪军,严理.南黄海西部“阿尼努德振动”现象的初步研究[J].海洋科学,1994,18(5):62-67. |
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| 作者姓名： | 于洪军 严理 |
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| 作者单位： | 中国科学院海洋研究所!青岛266071 |
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| 摘 要： | 通过对南黄海的大量浅地层部面仪资料的判读,发现在低于现代海面６０ｍ附近的地层中有２条古海岩线,从而证明了中国陆架上也曾发生过阿尼努德振动。这项发现对于进一步研究晚更新世末斯的陆架环境具有重要的意义。
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| 关 键 词： | 阿尼努德振动 南黄海 晚更新世末期 |
| 收稿时间： | 1993/4/20 0:00:00 |
THE INITIAL STUDY OF ALLEROD INTERSTADIAL IN THE SOUTH-WESTERN YELLOW SEA |
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| Yu Hongjun and Yan Li.THE INITIAL STUDY OF ALLEROD INTERSTADIAL IN THE SOUTH-WESTERN YELLOW SEA[J].Marine Sciences,1994,18(5):62-67. |
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| Authors: | Yu Hongjun and Yan Li |
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| Abstract: | Based on the available data of Northern Europe, there were short interstadial phases of warming (800yr) occurred once in the last stage of Late Pleistocene. This appearance is called "Allerod Interstadial". The author studied a lot of shallow layer profiler records in the Southern Yellow Sea and found two Paleocoastlines in the marine stratum of lower 60m than today's sealever. It proves the Allerod Interstudial once occurred in China continental shelf. This discover is very important to advanced study about the shelf environment in the last stage of lute Pleistocene. |
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| Keywords: | Allerod Interstadial the South-western Yellow Sea the last stage of Late Pleistocene |
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