Magnetic Susceptibility in Surface Sediments in the Southern South China Sea and Its Implication for Sub-sea Methane Venting

Zhong Chen; Wen Yan; Xianzan Tang; Jianguo Liu; Muhong Chen; Huaping Yang

doi:10.1007/s12583-009-0019-y

Volume 20 Issue 1

Feb 2009

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Journal of Earth Science > 2009 > 20(1): 193-204.

Zhong Chen, Wen Yan, Xianzan Tang, Jianguo Liu, Muhong Chen, Huaping Yang. Magnetic Susceptibility in Surface Sediments in the Southern South China Sea and Its Implication for Sub-sea Methane Venting. Journal of Earth Science, 2009, 20(1): 193-204. doi: 10.1007/s12583-009-0019-y

Citation:

Zhong Chen, Wen Yan, Xianzan Tang, Jianguo Liu, Muhong Chen, Huaping Yang. Magnetic Susceptibility in Surface Sediments in the Southern South China Sea and Its Implication for Sub-sea Methane Venting. Journal of Earth Science, 2009, 20(1): 193-204. doi: 10.1007/s12583-009-0019-y

Citation:

Zhong Chen, Wen Yan, Xianzan Tang, Jianguo Liu, Muhong Chen, Huaping Yang. Magnetic Susceptibility in Surface Sediments in the Southern South China Sea and Its Implication for Sub-sea Methane Venting. Journal of Earth Science, 2009, 20(1): 193-204. doi: 10.1007/s12583-009-0019-y

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Magnetic Susceptibility in Surface Sediments in the Southern South China Sea and Its Implication for Sub-sea Methane Venting

doi: 10.1007/s12583-009-0019-y

1.
Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
2.
College of Chemical Engineering and Materials Science, Zhuhai Campus of Beijing Institute of Technology, Zhuhai 519085, China

Funds:

the CAS Knowledge Innovation Program KZCX2-YW-211

the National Natural Science Foundation of China 40676038

Scientific and Technical Supporting Programs Funded by the Ministry of Science & Technology of China 2006BAB19B03

More Information

Corresponding author: Chen Zhong, chzhsouth@scsio.ac.cn
Received Date: 28 Oct 2008
Accepted Date: 01 Dec 2008

Abstract

Abstract

In order to understand the characteristics of magnetic variability and their possible implication for sub-sea methane venting, magnetic susceptibility (MS) of 145 surface sediment samples from the southern South China Sea (SCS) was investigated. Magnetic particles extracted from 20 representative samples were also examined for their mineral, chemical compositions and micromorphology. Results indicate that MS values range between −7.73×10⁻⁸ and 45.06×10⁻⁸ m³/kg. The high MS zones occur at some hydrocarbon-bearing basins and along main tectonic zones, and low ones are distributed mainly within the river delta or along continental shelves. Iron concretions and manganese concretions are not main contributors for high MS values in sediments, while authigenic iron sulphide minerals are possibly responsible for the MS enhancement. This phenomenon is suspected to be produced by the reducing environment where the high upward venting methane beneath the seafloor reacts with seawater sulfate, resulting in seep precipitation of highly susceptible intermediate mineral pyrrhotite, greigite and paramagnetic pyrite. It suggests that MS variability is possibly one of the geochemical indicators for mapping sub-sea zones of methane venting in the southern SCS.
- magnetic susceptibility,
- magnetic particle,
- oil/gas & gas hydrate,
- surface sediment,
- southern South China Sea

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References(49)

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