Upwelling and sedimentation dynamics

Hu Dunxin

doi:10.1007/BF02888388

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Upwelling and sedimentation dynamics

OriginalPaper | Updated：2023-05-16

- Upwelling and sedimentation dynamics
- Upwelling and sedimentation dynamics
- 海洋湖沼学报（英文） 1984年2卷第1期页码：12-19
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 999 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02888388
  中图分类号：
- 纸质出版：1984
- Accepted：
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Upwelling and sedimentation dynamics[J]. 海洋湖沼学报（英文）, 1984,2(1):12-19.

Dunxin, H. Upwelling and sedimentation dynamics., Chin. J. Ocean. Limnol. 2, 12–19 (1984). https://doi.org/10.1007/BF02888388
Upwelling and sedimentation dynamics[J]. 海洋湖沼学报（英文）, 1984,2(1):12-19. DOI： 10.1007/BF02888388.

Dunxin, H. Upwelling and sedimentation dynamics., Chin. J. Ocean. Limnol. 2, 12–19 (1984). https://doi.org/10.1007/BF02888388 DOI：

摘要

Abstract

It is found that the mud distributions in the Huanghai Sea and East China Sea are extremely identical with the upwelling's in terms of locality and extent. The process of the mud formation is examined. It is concluded that vertical circulation i.e. upwelling plays a determinant role in the process and furthermore

it is inferred that wherever upwelling occurs on continental shelf

mud should be formed and

conversely

wherever downwelling takes place

mud should not exist

for which coarse sediment should substitute.

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Keywords

references

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