南海表层沉积物中细粒组分的稀土元素地球化学特征

刘建国; 陈忠; 颜文; 陈木宏; 殷学博

doi:10.3799/dqkx.2010.072

Volume 35 Issue 4

Jul. 2010

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Article Navigation > Earth Science > 2010 > 35(4): 563-571

LIU Jian-guo, CHEN Zhong, YAN Wen, CHEN Mu-hong, YIN Xue-bo, 2010. Geochemical Characteristics of Rare Earth Elements in the Fine-Grained Fraction of Surface Sediment from South China Sea. Earth Science, 35(4): 563-571. doi: 10.3799/dqkx.2010.072

Citation:

LIU Jian-guo, CHEN Zhong, YAN Wen, CHEN Mu-hong, YIN Xue-bo, 2010. Geochemical Characteristics of Rare Earth Elements in the Fine-Grained Fraction of Surface Sediment from South China Sea. Earth Science, 35(4): 563-571. doi: 10.3799/dqkx.2010.072

Citation:

LIU Jian-guo, CHEN Zhong, YAN Wen, CHEN Mu-hong, YIN Xue-bo, 2010. Geochemical Characteristics of Rare Earth Elements in the Fine-Grained Fraction of Surface Sediment from South China Sea. Earth Science, 35(4): 563-571. doi: 10.3799/dqkx.2010.072

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Geochemical Characteristics of Rare Earth Elements in the Fine-Grained Fraction of Surface Sediment from South China Sea

doi: 10.3799/dqkx.2010.072

1.
Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
2.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

Received Date: 2009-11-20
Publish Date: 2010-07-01

Abstract

Abstract

Rare earth elements (REE) in the fine-grained fraction of surface sediments were detected by ICP-MS analysis, to study distribution characters of REE and the influencing factors in the South China Sea. Results reveal that distribution of REE in sediments is mainly related with continental input, biological effects and provision of volcanic materials in the South China Sea. The REE NASC normalization distribution pattern of average fine-grained fraction in the South China Sea is similar to that in Chinese loess, and also those of coastal rivers including the Pearl River and Mekong River, but sharply different from that of Cenozoic basalts from the South China Sea, indicating that fine-grained fraction was mostly derived from the mainland substance. Trend analysis of REE indicates that fine-grained fraction between the Pearl River Mouth and the southern Hainan Island was transported into the slope in the southeastern direction, while sediments between the southwestern Taiwan Island and the Pearl River Mouth were mostly transported southward. Sediments in the western Luzon Island and near the Huangyan Island were mainly conveyed northwestward, which could reach 113°E in the west and 20°N in the north. In the southern South China Sea, sediments were wholly transported towards the northwestern Nansha trough.
- rare earth elements,
- geochemistry,
- surface sediments,
- fine-grained fraction,
- trend analysis,
- South China Sea

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References(50)

References

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Geochemical Characteristics of Rare Earth Elements in the Fine-Grained Fraction of Surface Sediment from South China Sea

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