An approach to the transgressive sedimentary pattern of the present continental shelf

Lin Hejie; Huang Xingzhen; Pan Zhonghai; Li Chengxian

doi:10.1007/BF02845000

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An approach to the transgressive sedimentary pattern of the present continental shelf

OriginalPaper | Updated：2023-05-16

- An approach to the transgressive sedimentary pattern of the present continental shelf
- An approach to the transgressive sedimentary pattern of the present continental shelf
- 海洋湖沼学报（英文） 1987年5卷第2期页码：161-171
- Affiliations：
  
  Lanzhou Institute of Geology Academia Sinica
- Author bio：
- Funds：
  
  This paper was published in Chinese in;Ocean. Limn. Sin.;15;(2):179–187, 1984
- DOI：10.1007/BF02845000
  中图分类号：
- 纸质出版：1987
- Accepted：
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An approach to the transgressive sedimentary pattern of the present continental shelf[J]. 海洋湖沼学报（英文）, 1987,5(2):161-171.

Hejie, L., Xingzhen, H., Zhonghai, P. et al. An approach to the transgressive sedimentary pattern of the present continental shelf., Chin. J. Ocean. Limnol. 5, 161–171 (1987). https://doi.org/10.1007/BF02845000
An approach to the transgressive sedimentary pattern of the present continental shelf[J]. 海洋湖沼学报（英文）, 1987,5(2):161-171. DOI： 10.1007/BF02845000.

Hejie, L., Xingzhen, H., Zhonghai, P. et al. An approach to the transgressive sedimentary pattern of the present continental shelf., Chin. J. Ocean. Limnol. 5, 161–171 (1987). https://doi.org/10.1007/BF02845000 DOI：

摘要

Abstract

On the basis of our study of the present sediments in the northern part of the continental

shelf of the South China Sea

this article clarifies our views that a “three-zone pattern” is the basic feature of transgression-type sedimentation. The classification of transgression-type sedimentation of the present continental shelf is based on: the close relationships between the formation of the present continental shelf and the position of the low sea level of the Würm glacial stage

the genetic types and environmental features of sedimentary zoning

the relationship between the formation of glauconite with different maturity and the migration of coastline

the speed of tranagression

and the overlying speed of sedimentation. We put forward the genetic name of the “three-zone pattern” to denote: All these are of significance to the study of fossil marine strata.

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references

Lanzhou Institute of Geology, Academia Sinica, 1982, “Sedimentological Study on the Present Sediment in the Northern Part of the South China Sea Continental Shelf”, Papers on Petroleum Geology, People's Publishing House of Ganou. pp. 99–132 (in Chinese)

Wang Jingtai, Wang Pinxian, 1960. “Relationship between Eustasy and Climate Change in East China since the Late Pleistocene Epoch”,Acta Geographica Sinica 35(4):299–312. (in Chinese)

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