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南黄海东部泥区沉积速率和物源探讨
DISCUSSION ON SEDIMENTATION RATES AND MATERIAL SOURCE IN THE EAST PART OF THE SOUTH YELLOW SEA
【摘要】 根据测定岩芯中210Pb放射性活度,南黄海东部泥区最高现代沉积速率为1.65 cm/a,泥区边缘沉积速率为0.12cm/a。表层沉积物中的化学成分CaCO3,Cu,Sr,Ti和Rb的 含量表明黄河物源对该泥区没有影响,长江物源对该区贡献较小。
【Abstract】 The sedimentation rates in the east part of the South Yellow Sea were determined based on profiles of 210Pb in the cores. It ranges from 0. 12 to 1. 65 cm/a. In order to discuss material sources of fine-grained mud in the eastern South Yellow Sea, Chemical elements CaCO3,Sr,Cu,Ti and Rb have been determined. The contents of CaCO3 and Sr showed that the Huanghe River materials could hardly be transported to the eastern South Yellow Sea. The contents of Cu,Ti and Rb showed that parts of terrigenous materials from the Changjiang River were transported to the mud areas. This research was supported by the National Natural Science Foundation of China and Korea.
【Key words】 Sedimentation rates; Material sources; Eastern South Yellow Sea;
- 【文献出处】 海洋科学 ,MARINE SCIENCES , 编辑部邮箱 ,1999年05期
- 【分类号】P736.2
- 【被引频次】28
- 【下载频次】301