| 对我国沿海全新世海面变化研究的讨论 |
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| 引用本文： | 薛春汀.对我国沿海全新世海面变化研究的讨论[J].海洋学报,2002,24(4):58-67. |
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| 作者姓名： | 薛春汀 |
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| 作者单位： | 青岛海洋地质研究所, 山东, 青岛, 266071 |
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| 摘 要： | 距今6 000a的高海面及其后海面波动论点的主要依据是对渤海西岸贝壳堤、华南海岸海滩岩和珊瑚礁、天津市宁河县俵口牡蛎礁剖面和江苏北部建湖县庆丰剖面的研究,然而这些资料无法证明高海面和海面波动,因为珊瑚礁、牡蛎礁、贝壳堤、海滩岩和潮滩沉积物都不能提供古海平面的精确信息.
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| 关 键 词： | 全新世 海面变化 沉积环境 贝壳堤 庆丰剖面 |
| 文章编号： | 0253-4193(2002)04-0058-10 |
| 收稿时间： | 8/8/2001 12:00:00 AM |
| 修稿时间： | 2001年8月8日 |
Holocene sea-level change along China coast |
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| XUE Chun-ting.Holocene sea-level change along China coast[J].Acta Oceanologica Sinica (in Chinese),2002,24(4):58-67. |
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| Authors: | XUE Chun-ting |
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| Affiliation: | Qingdao Institute of Marine Geology, Qingdao 266071, China |
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| Abstract: | The bases of the viewpoint of higher sea level in 6 000 aBP and sea level fluctuation since then are the shell ridges on the west coast of the Bohai Sea, beachrock and coral reefs on South China coast, the Holocene stratigraphic section at Biaokou Village, Ninghe County, Tianjin Municipality and Qingfeng section in Jianhu County, Jiangsu Province. However, the above data cannot provide such evidences, because the coral reef, oyster reef, shell ridge, beachrock and tidal flat deposits cannot provide information of such accurate sea level changes. |
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| Keywords: | Holocene sea level change sedimentary environment shell ridge Qinfeng section |
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