Rare earth elements in sediments of the China continental shelf

Zhao Yiyang; Wang Jintu; Qin Zhaoyang; Chen Yuwei; Wang Xianjue; Wu Mingqing

doi:10.1007/BF02842659

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Rare earth elements in sediments of the China continental shelf

OriginalPaper | Updated：2023-05-16

- Rare earth elements in sediments of the China continental shelf
- Rare earth elements in sediments of the China continental shelf
- 海洋湖沼学报（英文） 1989年7卷第1期页码：70-78
- Affiliations：
  
  1. Institute of Oceanology
  2. Institute of Geochemistry
- Author bio：
- Funds：
  
  Contribution No. 1520 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02842659
  中图分类号：
- 纸质出版：1989
- Accepted：
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Rare earth elements in sediments of the China continental shelf[J]. 海洋湖沼学报（英文）, 1989,7(1):70-78.

Yiyang, Z., Jintu, W., Zhaoyang, Q. et al. Rare earth elements in sediments of the China continental shelf., Chin. J. Ocean. Limnol. 7, 70–78 (1989). https://doi.org/10.1007/BF02842659
Rare earth elements in sediments of the China continental shelf[J]. 海洋湖沼学报（英文）, 1989,7(1):70-78. DOI： 10.1007/BF02842659.

Yiyang, Z., Jintu, W., Zhaoyang, Q. et al. Rare earth elements in sediments of the China continental shelf., Chin. J. Ocean. Limnol. 7, 70–78 (1989). https://doi.org/10.1007/BF02842659 DOI：

摘要

Abstract

Determination of the concentrations of

15 rare earth elements (REE) in China continental shelf sediments by X-ray fluorescent spectral analysis of selected representative sediment samples showed that REE concentration in the sediments is 156 ppm

similar to that in China loess and Fujian granite

but different from that in Pacific sediments. The shelf REE have the characteristic distribution pattern of typical continental crust REE and evidently philo-continental property. The above findings suggest that weathered materials transported from the China continent are the main source of the REE in China continental shelf sediments. Experiments show that REE exist mainly in the crystal lattices of clay minerals (<2μ) as isomorphs and that REE have close relation with most elements (Al

etc.) related with clay minerals

but have negative correlation with the biophile elements Ca and Sr.

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references

Chen Lirong et al., 1986. An approach to the detrital mineral assemblages and their distribution patterns in the sedi ments of the China Seas.Acta Oceanologica Sinica 8 (3): 87–96. (in Chinese with English abstract)

Liu Dongsheng et al., 1985. Loess and Environment. Science Press, Beijing, pp. 256–264. (in Chinese)

Wang Xianjue et al., 1982. REE geochemistry in sea—floor sediments in the continental shelf of the East China Sea.Geochimica 1: 56–65. (in Chinese with English abstract)

Wang Zhonggang et al., 1985. Mineral table of REE. Geology—Geochemistry (supplement): 65–68. (in Chinese)

Wu Mingqing, 1983. REE geochemistry of sea—floor sediments from the Taiwan Bank, ChinaGeochimica 3: 303–313. (in Chinese with English abstract)

Zhao Yiyang et al., 1983a. Geochemistry of some elements in sediments of the East China Sea.Chin. J. Oceanol. Limol. 1 (2): 210–222.

Zhao Yiyang et al., 1983b. Geochemical analysis of the sediments of the Yellow Sea.Oceanologia et Limnologia Sinica 14 (5): 432–446. (in Chinese with English abstract)

Zhao Yiyang et al., 1983c. Some geochemical characteristics of Zr and REE in sediments of the East China Sea.Kexue Tongbao 28 (11): 1532–1535.

Zhao Yiyang, 1985. Some geochemical patterns of shelf sediments of the China Seas.Chin. J. Oceanol. Limnol. 3 (2): 200–211.

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