Causative Mechanism of the Continental Margin Polymetallic Nodules from the South China Sea and its Resource Effects

Article Preview

Abstract:

Polymetallic nodules are one of the most important sedimentary mineral resources in the ocean, in which iron, manganese, copper, cobalt, nickel and other metals are rich, and rare earth elements are rich, too. The samples are collected from the northwest continental margin of South China Sea (SCS). Their model show the similar appearance to the oceanic nodules which collected from the Pacific and Indian Ocean. They are big, regular shape and clear layers. But their geochemical characteristics show distinct difference with oceanic nodules.The samples formed by multiple millimeter-thick layers of Fe and Mn oxyhydroxides surrounding the nucleus composed of plastic marl and sediment. Massive, laminated, detrital and mottled to dendritic textural features were developed by the Fe and Mn oxyhydroxide layers.Based on the detailed study of the geochemistry and growth rate, the nodules may represent new-type ones which grow fastly in high sediment rates environment from the northwest continental margin of the SCS. The reason of the fast growth may be affected by the environmental fluctuations and the change of terrigenous sediments. Elements correlation of Mn-Fe-(Cu+Ni) suggests that the origin of the sample may be of hydrogenic. It may be show that these nodules are dominative of the special environment of the marginal sea which includes the geographical condition and the oceanic environmental factors. The average content of Rare Earth Elements (REEs) in these samples are much higher than those recorded in Earth’ crust and sedimentary rocks. The enrichment of rare earth elements is controlled by iron and manganese oxides and clay minerals in nodules, which could absorb rare earth elements from seawater and terrigenous sediment. Ce elements are highly enriched, making polymetallic nodules become the first used rare earth elements in oceanic mineral development.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 524-527)

Pages:

408-412

Citation:

Online since:

May 2012

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2012 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] J.P. Kennett and N.D. Watkins. Science, Vol.188 (1975), p.1011

Google Scholar

[2] A.V. Philomène, S. C. David and L. M. Charles. Progress In Oceanography, Vol. 3(2004), p.125

Google Scholar

[3] X.J. Wang, Y.W. Chen and M.Q. Wu. Oceanologia et Limnologia Sinica, Vol. 6(1984), p.501

Google Scholar

[4] G.D. Bao and Q.X. Li. Oceanologia et Limnologia Sinica, Vol.3 (1993), p.304

Google Scholar

[5] Y.W. Chen and X.T. Gui. Benjing: Science and Technology Press. (1998)

Google Scholar

[6] Z.H. Lin, F.W.Ji, F.Y. Zhang, et al. Marine Geology & Quaternary Geology, Vol. 3(2003), p.7

Google Scholar

[7] S.L. Li. Acta Oceanologica Sinica, Vol.3 (2001), p.127

Google Scholar

[8] South China Sea Institute of Oceanology, Chinese Academy of Science. Integrated surveying report of the South China Sea (I).Science Press, Beijing, (1985)

Google Scholar

[9] Z.G. Zhang, N.Q. Fang, Y.S. Du, et al. Marine Geology & Quaternary Geology, Vol.4 (2008), p.55

Google Scholar

[10] Z.G. Zhang, N.Q. Fang, Y.S. Du, et al. Earth Science, Vol.6 (2009), p.61

Google Scholar

[11] N. Florence, J. Peter and M. Matt. Marine Chemistry,Vol.104 (2007),p.156

Google Scholar

[12] D.Y.Xu, Q.H. Jin, D.H. Liang, et al. Beijing: Geologic Publishing House (1994)

Google Scholar

[13] D.Y.Xu. Beijing: Geologic Publishing House (1995)

Google Scholar

[14] F. H.Zhu. Marine Geology Letters, Vol.4 (2006), p.15

Google Scholar