Chinese Science Bulletin

, Volume 48, Supplement 1, pp 30–36 | Cite as

Sediment provenance and province of the southern Yellow Sea: Evidence from light mineral

  • Kunshan Wang
  • Xuefa Shi
  • Xiaoli Jiang


The distribution for percent content of light mineral is divided in detail to emphasize distributional trends of higher and lower contents by using 222 samples of light mineral in the southern Yellow Sea. 5 mineral provinces are divided, and they are I -north mineral province of the southern Yellow Sea, the sediment dominantly derived from the Yellow River; II-mixed mineral province, the sediment derived from both the Yellow River and Yangtze River; Illmiddle mineral province, the sediment derived mainly from the Yellow River and a part of sediment derived from Yangtze River; IV-province east of Yangtze River mouth, the sediment derived dominantly from Yangtze River; and V-south mineral province, sediment was affected by relict sediment and modern sediment of Yangtze River. In this paper, the assemblage of dominant mineral and diagnostic mineral for the five provinces are discerned.


southern Yellow Sea light mineral mineral provinces material source 


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  1. 1.
    Schafer, J., Wolfgang, D., Heavy-mineral analysis and typology of detritus zircon: A new approach to provenance study, Journal of Sediment Research, 1997, 67(3): 451–461.Google Scholar
  2. 2.
    Uddin, A., Lundberg, N., Unroofing history of the eastern Himalaya: heavy-mineral study of Cenozoic sediments from the Bengal Basin, Bangladesh, Journal of Sediment Research, 1998, 68(3): 465–472.Google Scholar
  3. 3.
    Vital, H., Stattegger, K., Garbe-Schonberg, C., Composition and trace-element geochemistry of detrital clay and heavy-mineral suits of the lowermost Amazon River: A provenance study, Journal of Sediment Research, 1999, 69(3): 563–575.Google Scholar
  4. 4.
    Jeffry, D. G., Detrital magnetite as a provenance indicator, Journal of Sedimentary Petrology, 1990, 60(6): 940–951.Google Scholar
  5. 5.
    Stephanie, J. S., Detrital opaque oxides as provenance indicators in River Nile sediment, Journal of Sediment Research, 1995, 65(4): 668–674.Google Scholar
  6. 6.
    Graham, I. J., Glasby, G. P., Churchman, G. J., Provenance of the detrital component of deep-sea sediments from the Sw Pacific ocean based on mineralogy, geochemistry and Sr isotopic composition, Marine Geology, 1997, 140: 75–96.CrossRefGoogle Scholar
  7. 7.
    Liou, M. H., Wu, S. Y., Wang, Y. J., Late Quaternary Period Sedimentation of Yellow Sea (in Chinese), Beijing: China Ocean Press, 1987, 69–71.Google Scholar
  8. 8.
    Qin, Y. S., Zhao, Y. Y., Chen, L. R. et al., Geology of the Yellow Sea (in Chinese), Beijing: Ocean Press, 1989, 100–102.Google Scholar
  9. 9.
    Chen, L. R., Study on the mineral assemblage of the Bohai Sea, Yellow Sea and East China Sea, Marine Sciences (in Chinese), 1989, 2: 1–7.Google Scholar
  10. 10.
    Chen, L. R., Xu, W. Q., Shen, S. X., A study on the light mineral in the sediments of the East China Sea, Studia Marina Sinica (in Chinese), 1984, (21): 297–304.Google Scholar
  11. 11.
    Zhao, Y. Y., Yan, M. C., Geochemistry of Sediments of the Chinese Shallow Sea (in Chinese), Beijing: Science Press, 1994, 1–17.Google Scholar
  12. 12.
    Yang, Y. H., Cao, X. Y., Liou, S. H. et al., Mathematic Methods of Geology (in Chinese), Shenyang: Eastnorth China Normal University Press, 1992, 1–24, 71–174.Google Scholar
  13. 13.
    Lu, W. D., Zhu, Y.L., Sha, J. et al., SPSS for Windows from Rudiment to Proficiency (in Chinese), Beijing: Publishing House of Electronics Industry, 1997.Google Scholar

Copyright information

© Science in China Press 2003

Authors and Affiliations

  1. 1.Institute of OceanologyChinese Academy of SciencesQingdaoChina
  2. 2.Key Laboratory of Marine Sedimentology and Environmental GeologyState Oceanic AdministrationQingdaoChina
  3. 3.Graduate SchoolChinese Academy of SciencesBeijingChina

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