Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (1): 261-277.doi: 10.13278/j.cnki.jjuese.20180133

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Comparison Between the Marginal-Sea Polymetallic Nodules in South China Sea and Ocean Polymetallic Nodules

Yin Zhengxin1, Wang Haifeng2, Han Jinsheng3, Lü Xiuya1, Shen Zezhong1, Chen Jing1, He Huizhong1, Xie Anyuan1, Guan Yao2,3,4, Dong Chao1,5   

  1. 1. South China Sea Marine Survey and Technology Center, State Oceanic Administration, Guangzhou 510275, China;
    2. Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou 510075, China;
    3. Key Laboratory of Mineralogy and Metallogeny, Chinese Academy of Sciences, Guangzhou 510640, China;
    4. Fourth Institute of Oceanography, Ministry of Natural Resources, Beihai 536000, Guangxi, China;
    5. Key Laboratory of Technology and Application for Safeguarding of Marine Rights and Interests, State Oceanic Administration, Guangzhou 510275, China
  • Received:2018-05-25 Published:2019-01-18
  • Supported by:
    Supported by Open Project Fund of Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources (KLMMR-2017-B-02), Marine Public Welfare Industry Research Projects (201505002), Marine Science and Technology of South China Sea Branch,SOA Director Fond (1619), National Marine Geology Special Project of China (DD20160147, DD20189643), National Natural Science Foundation of China(41706055) and Cooperation Project Fund of Key Laboratory of Mineralogy and Metallogeny, Chinese Academy of Sciences (KLMM20170203)

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Abstract: With the discovery of more and more polymetallic nodule mineralization zones in the South China Sea (SCS) in recent years, the researches of marine polymetallic nodules in this area have become deeper. The SCS marginal-sea polymetallic nodules have their own unique characteristics, which are very different from those in the oceanic environment. Based on the comparative analysis of the previous research results, the authors studied the metallogenetic characteristics of the SCS polymetallic nodules, and provided theoretical guidance for the evaluation of the SCS submarine polymetallic mineral resources. The results show that the mineral composition of the SCS marginal nodules is basically similar to that of oceanic nodules, mainly composed of Mn-and Fe-phase minerals, but the SCS nodules contain a large amount of silicate minerals, indicating that they are greatly affected by terrestrial detrital minerals. Compared to the oceanic nodules in the main economic mineralization zones, the content of the main economic elements such as Mn, Cu, Co, Ni and Zn in the SCS nodules are relatively low, while the contents of terrestrial-derived elements such as Fe, Ti, P, Nb, Pb, Rb, Sc, Ta, Sr, Th and REY (REE and Y) are relatively high. The elemental geochemical characteristics and REE shale-normalized patterns of the SCS polymetallic nodules show that they are of hydrogenetic origin with lower Mn/Fe ratios, high average growth rate, and relatively higher positive δCe anomalies, indicating that the SCS nodules grew in more oxidizing seawater environment. Although the high sediment accumulation rate and turbulent seawater environment affect the mineralization of the SCS nodules, the entry of a large number of terrestrial material provides a rich source of metallogenetic material for the rapid growth of nodules. The SCS marginal polymetallic nodules are rich in a variety of economic metal elements, and can be used as potential marine mineral resources.

Key words: polymetallic nodules, metallogenic characteristics, mineral compositions, element geochemistry, Marginal-Sea in South China Sea, Oceans

CLC Number: 

  • P618.3
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