On the source and genesis of the mud in the central area of the South Yellow Sea

Zhao Yiyang; Qin Zhaoyang; Li Fengye; Chen Yuwei

doi:10.1007/BF02846453

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On the source and genesis of the mud in the central area of the South Yellow Sea

OriginalPaper | Updated：2023-05-16

- On the source and genesis of the mud in the central area of the South Yellow Sea
- On the source and genesis of the mud in the central area of the South Yellow Sea
- 海洋湖沼学报（英文） 1990年8卷第1期页码：66-73
- Affiliations：
  
  1. Institute of Oceanology
  2. Institute of Geochemistry
- Author bio：
- Funds：
  
  Project supported by the National Natural Science Foundation of China, contribution No. 1646 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02846453
  中图分类号：
- 纸质出版：1990
- Accepted：
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On the source and genesis of the mud in the central area of the South Yellow Sea[J]. 海洋湖沼学报（英文）, 1990,8(1):66-73.

Yiyang, Z., Zhaoyang, Q., Fengye, L. et al. On the source and genesis of the mud in the central area of the South Yellow Sea., Chin. J. Ocean. Limnol. 8, 66–73 (1990). https://doi.org/10.1007/BF02846453
On the source and genesis of the mud in the central area of the South Yellow Sea[J]. 海洋湖沼学报（英文）, 1990,8(1):66-73. DOI： 10.1007/BF02846453.

Yiyang, Z., Zhaoyang, Q., Fengye, L. et al. On the source and genesis of the mud in the central area of the South Yellow Sea., Chin. J. Ocean. Limnol. 8, 66–73 (1990). https://doi.org/10.1007/BF02846453 DOI：

摘要

Abstract

Investigations and studies for years all demonstrated that there is a patch of fine-grained mud in the central area of the South Yellow Sea. However

scientists have different opinions on its material source

genesis

and sedimentation intensity. Some believe that the materials come from the Huanghe River

some think that the mud area represents the depocentre of the South Yellow Sea

and some consider it as “relict mud”. The authors' geochemical study reveals that the mud is multi-sourced

yet the material supply is not ample

and that a little amount of fine-grained suspended materials deposited slowly under the dynamic action of a cyclonic gyre formed the modern muddy sediment

which is named “multi-source modern mud”.

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references

Hu Dunxin, 1984. Upwelling and sedimentation dynamics.Chinese Journal of Oceanology and Limnology 2(1): 12–19.

Liu Houmin, Wu Shiying and Wang Yongji, 1987. The Yellow Sea Late Quaternary Sediment. China Ocean Press. pp. 24–115.

Qin Yunshan and Li Fan, 1986. Study of the influence of sediment loads discharged from Huanghe River on sedimentation in the Bohai and Yellow Seas.Studia Marina Sinica.27: 125–135. (In Chinese, with English abstract)

Qin Yunshan, Zhao Yiyang, Zheng Tiemin, Tang Baojue and J. D. Milliman, 1988. A study of shallow acoustic stratigraphy in the south Huanghai Sea.Oceanologia et Limnologia Sinica.19 (5): 401–409. (In Chinese, with English abstract)

Shen Shunxi, Chen Lirong and Xu Wenqiang, 1984. Mineral assemblage and their distribution patterns in the sediments of the Huanghai Sea.Oceanologia et Limnologia Sinica.15 (3): 240–250. (In Chinese, with English abstract)

Yang Guangfu, Dong Tailu and Xu Shanmin, 1984. A general description of the modern deposition on the continental shelf of the East China Sea.Studia Marina Sinica.21:281–290. (In Chinese, with English abstract)

Zhao Yiyang and Qian Jiangchu, 1981. The U.S. isotope210Pb determination of geologic chronology.Marine Sciences.3:44–45. (In Chinese)

Zhao Yiyang, He Lijuan and Chen Yuwei, 1989. On regional distribution patterns of elements in sediments of the Yellow Sea.Marine Sciences.1:1–5. (In Chinese, with English abstract)

Zhao Yiyang, Li Fengye and han Guirong, 1989. Chemical Differences among Various Sediments of the Yellow Sea. Development in Geoscience. Science Press. pp. 321–329.

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