Sediment provenance and distribution in Caofeidian, Bohai Bay, revealed by offshore detrital mineral analysis

HU Yanbin; FENG Yongcai; HAO Liancheng; YANG Kaili; PANG Guotao; WANG Kechao; LIU Jian

doi:10.16028/j.1009-2722.2024.161

2024 Vol. 40, No. 11

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Article navigation > Marine Geology Frontiers > 2024 > 40(11): 70-79

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HU Yanbin, FENG Yongcai, HAO Liancheng, YANG Kaili, PANG Guotao, WANG Kechao, LIU Jian. Sediment provenance and distribution in Caofeidian, Bohai Bay, revealed by offshore detrital mineral analysis[J]. Marine Geology Frontiers, 2024, 40(11): 70-79. doi: 10.16028/j.1009-2722.2024.161

Citation:

HU Yanbin, FENG Yongcai, HAO Liancheng, YANG Kaili, PANG Guotao, WANG Kechao, LIU Jian. Sediment provenance and distribution in Caofeidian, Bohai Bay, revealed by offshore detrital mineral analysis[J]. Marine Geology Frontiers, 2024, 40(11): 70-79. doi: 10.16028/j.1009-2722.2024.161

Sediment provenance and distribution in Caofeidian, Bohai Bay, revealed by offshore detrital mineral analysis

Yantai Center of Coastal Zone Geological Survey, China Geological Survey, Yantai 264000, China

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Corresponding author: HAO Liancheng, 251035203@qq.com

Received Date: 12 July 2024

Publish Date: 28 November 2024

Abstract

Abstract

A comparative study on detrital minerals from 161 surface sediments in Caofeidian, Bohai Bay, was conducted to understand the sediment provenance and distribution. Eleven types of light minerals and 27 types of heavy minerals were identified in the study area. The light minerals were mainly feldspar, quartz, and flake minerals, with an average mass percentage of 82.2%. The heavy minerals consisted of predominantly hornblende, epidote, and authigenic pyrite. Based on the distribution characteristics and cluster analysis of detrital minerals, the study area could be divided into three sedimentary regions: the Luanhe River mineral region, the mixed source region, and the Yellow River mineral region. We concluded that provenance is the main factor controlling the assemblage and distribution of detrital minerals in the study area, and the land reclamation activities have changed the hydrodynamic and sedimentary environment in Caofeidian, and further affected the distribution characteristics of detrital minerals.
- Caofeidian /
- detrital mineral /
- provenance /
- hydrodynamic environment /
- land reclamation

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References

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