Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin

Li Fan; Zhuang Jiezao; Yu Jianjun; Du Quansheng; Dong Tailu; Jiang Xiuhang

doi:10.1007/BF02849663

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Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin

OriginalPaper | Updated：2023-05-16

- Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin
- Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin
- 海洋湖沼学报（英文） 1990年8卷第3期页码：240-248
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
- DOI：10.1007/BF02849663
  中图分类号：
- 纸质出版：1990
- Accepted：
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Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin[J]. 海洋湖沼学报（英文）, 1990,8(3):240-248.

Fan, L., Jiezao, Z., Jianjun, Y. et al. Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin., Chin. J. Ocean. Limnol. 8, 240–248 (1990). https://doi.org/10.1007/BF02849663
Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin[J]. 海洋湖沼学报（英文）, 1990,8(3):240-248. DOI： 10.1007/BF02849663.

Fan, L., Jiezao, Z., Jianjun, Y. et al. Buried paleo-channel system and records of sea level changes on the continental shelf in Yingge Sea Basin., Chin. J. Ocean. Limnol. 8, 240–248 (1990). https://doi.org/10.1007/BF02849663 DOI：

摘要

Abstract

High resolution geophysical instruments were used to locate many buried paleo-channels

paleo-lakes

and river mouth paleo-deltas formed during low sea level at the end of Late Pleistocene and Early Holocene. Some paleo-rivers flowed southward into the paleo-lake and others southeastward into the Paleo-South China Sea. It may be inferred from data on buried paleo-channels that sea level remained for some time at the −50m (longest time here)

−100m

and −130 to −140 m (lowest level) water depths

and that corresponding paleo-coastlines were formed at the respective depths.

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references

Chen Junren, 1983a. Study on paleo-coastline at 20 m water depth in the northern part of the South China Sea.Nanhai Geologica Studia, (2): 83–94. (In Chinese).

Chen Junren, 1983b. Study on paleo-coastline at 50 m water depth in the northern part of the South China Sea.Acta Geographica Sinica, (2): 176–187. (In Chinese, English abstract).

Feng Wenke, 1983. Remains of the coastal terraces and paleo-coastline in part of the South China Sea,Nanhai Geologica Studia, (2): 15–24. (In Chinese).

Huang Jinsen, 1979. The change of sea level since Late Pleistocene in the South China Sea.Nanhai Studia Marina Sinica 1, (In Chinese, with English abstract).

Lin Meihua 1981. Topography in the East China Sea.Marine Sciences, (1): 24–27. (In Chinese).

Qin Yunshan, 1986. Buried paleo-channel system in the East China Sea.Kexue Tongbao,24: 1887–1890. (In English).

Sukekatsu, 1982. To view the change of sea level in the Japan Sea based on topography on sea floor. After “The Change of Sea level”. pp. 120–140.

Sun Jiasong 1985. Unstable factories and influences on the ocean constructions in the eastern area of the China Sea.Marine Geology and Quarternary Geology,5(4): 21–30. (In Chinese, with English abstract).

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