Sedimentary evolution of modern Huanghe River delta lobe

Xue Chun-ting; D. J. Beets; Li Guang-xue; M. Peersman

doi:10.1007/BF02889466

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Sedimentary evolution of modern Huanghe River delta lobe

OriginalPaper | Updated：2023-05-16

- Sedimentary evolution of modern Huanghe River delta lobe
- Sedimentary evolution of modern Huanghe River delta lobe
- 海洋湖沼学报（英文） 1995年13卷第4期页码：325-331
- Affiliations：
  
  1. Geological Survey of the Netherlands
  2. Institute of Earth Science State University of Utrecht
- Author bio：
- Funds：
- DOI：10.1007/BF02889466
  中图分类号：
- 纸质出版：1995
- Accepted：
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Sedimentary evolution of modern Huanghe River delta lobe[J]. 海洋湖沼学报（英文）, 1995,13(4):325-331.

Chun-ting, X., Beets, D.J., Guang-xue, L. et al. Sedimentary evolution of modern Huanghe River delta lobe., Chin. J. Ocean. Limnol. 13, 325–331 (1995). https://doi.org/10.1007/BF02889466
Sedimentary evolution of modern Huanghe River delta lobe[J]. 海洋湖沼学报（英文）, 1995,13(4):325-331. DOI： 10.1007/BF02889466.

Chun-ting, X., Beets, D.J., Guang-xue, L. et al. Sedimentary evolution of modern Huanghe River delta lobe., Chin. J. Ocean. Limnol. 13, 325–331 (1995). https://doi.org/10.1007/BF02889466 DOI：

摘要

Abstract

The sedimentary history of a Huanghe (Yellow) River delta lobe can be divided into four stages. In the first stage

the crevasse splays and short-lived distributary channel deposits in the subaerial delta and sheet silt in the subaqueous delta were well developed. In the second stage

further differentiation of sedimentary environments occurred in the subaerial delta lobe (distributary channel

natural levee

flood plain

central lower delta plain and lateral lower delta plain) and the subaqueous delta lobe (prodelta

delta front and delta lateral). In the third stage

crevasse splay and short-lived distributary channel deposits mostly occurred in the lower or lower-middle part of the subaerial delta lobe

and sheet silt

accumulated off the river mouth. In the fourth stage

the abandoned lobe was reworked. The common vertical sequence of the modern Huanghe River delta showed alternating clayey silt and silt layers. A complete sequence from prodelta to upper delta plain was commonly composed of two or more delta lobes.

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references

Bronhold, B. D., Yang, Z. S., 1986. Sedimentary framework of the modern Huanghe (Yellow River) delta.Geo-Marine Letters 6: 77–83.

Cheng Guodong, 1987. Evolution and framework of the modern Huanghe River delta.Marine Geology and Quaternary Geology 7(suppl.): 7–18. (in Chinese with English abstract)

Cheng Guodong, Ren Yucan, 1986. Channel evolution and sedimentary sequence of modern Huanghe River delta.Marine Geology and Quaternary Geology 6(2): 1–15. (in Chinese with English abstract)

Peng Jiazhen, Si Shuheng, 1980. Fluvial process of the Huanghe River estuary II. hydrographical character and region of sediment silting.Oceanologia et Limnologia Sinica 11: 295–305 (in Chinese with English abstract)

Prior, D. B., Yang Z. S., 1986. The subaqueous delta of the modern Huanghe (Yellow River).Geo-Marine Letters 6: 67–75.

Wang Kaichen, 1985. The law of evolution of the Huanghe River estuary.In: Symposium on Dynamics Geomorphology and Sedimentation in Coast and Estuary. Science Press, Beijing, pp. 90–11. (in Chinese)

Wright, L. D., Wiseman, W. J., 1988. Marine dispersal and deposition of Yellow River silt by gravity-driven under-flowNature 332: 629–632.

Xue Chunting, Eisma, D. 1993. Depositional environment of lower delta plain of Yellow River delta.Marine Geology and Quaternary Geology 13(1): 33–40. (in Chinese with English abstract)

Xue Chunting, 1994. Division and recognition of modern Yellow River delta lobe.Geographical Research 14(2): 59–65 (in Chinese)

Ye Qingohao, 1982. The geomorphologic structure of the Yellow River delta and its evolution model.Acta Geographica Sinica 37: 349–363. (in Chinese with English abstract)

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