Rare earth elements in fine-grained sediments of major rivers from the high-standing island of Taiwan | |
Li, Chuan-Shun1; Shi, Xue-Fa1; Kao, Shuh-Ji2; Liu, Yan-Guang1; Lyu, Hua-Hua1; Zou, Jian-Jun1; Liu, Sheng-Fa1; Qiao, Shu-Qing1 | |
刊名 | JOURNAL OF ASIAN EARTH SCIENCES |
2013-06-05 | |
卷号 | 69页码:39-47 |
关键词 | Rare earth elements Taiwanese rivers Fluvial sediments Sediment provenance |
ISSN号 | 1367-9120 |
DOI | 10.1016/j.jseaes.2013.03.001 |
英文摘要 | Thirty-eight sediment samples from 15 primary rivers on Taiwan were retrieved to characterize the rare earth element (REE) signature of fluvial fine sediment sources. Compared to the three large rivers on the Chinese mainland, distinct differences were observed in the REE contents, upper continental crust normalized patterns and fractionation factors of the sediment samples. The average REE concentrations of the Taiwanese river sediments are higher than those of the Changjiang and Huanghe, but lower than the Zhujiang. Light rare earth elements (LREEs) are enriched relative to heavy rare earth elements (HREEs) with ratios from 7.48 to 13.03. We found that the variations in (La/Lu)(UCC)-(Gd/Lu)(UCC) and (La/Yb)(UCC)-(Gd/Yb)(UCC) are good proxies for tracing the source sediments of Taiwanese and Chinese rivers due to their distinguishable values. Our analyses indicate that the REE compositions of Taiwanese river sediments were primarily determined by the properties of the bedrock, and the intensity of chemical weathering in the drainage areas. The relatively high relief and heavy rainfall also have caused the REEs in the fluvial sediments from Taiwan to be transported to the estuaries down rivers from the mountains, and in turn delivered nearly coincidently to the adjacent seas by currents and waves. Our studies suggest that the REE patterns of the river sediments from Taiwan are distinguishable from those from the other sources of sediments transported into the adjacent seas, and therefore are useful proxies for tracing the provenances and dispersal patterns of sediments, as well as paleoenvironmental changes in the marginal seas. (c) 2013 Elsevier Ltd. All rights reserved. |
资助项目 | Special Basic Research Fund of the Central Public Research Institutes First Institute of Oceanography, State Oceanic Administration[GY02-2011G28] |
WOS关键词 | SMALL MOUNTAINOUS RIVERS ; EAST CHINA SEA ; CONTINENTAL-SHELF ; SOUTHWESTERN TAIWAN ; REE GEOCHEMISTRY ; FLUVIAL SEDIMENT ; AMAZON RIVER ; YELLOW SEA ; OCEAN ; PROVENANCE |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000319635400005 |
内容类型 | 期刊论文 |
源URL | [http://ir.fio.com.cn:8080/handle/2SI8HI0U/26696] |
专题 | 自然资源部第一海洋研究所 |
通讯作者 | Li, Chuan-Shun |
作者单位 | 1.State Ocean Adm, Inst Oceanog 1, Qingdao 266061, Peoples R China 2.Acad Sinica, Res Ctr Environm Changes, Taipei 11529, Taiwan |
推荐引用方式 GB/T 7714 | Li, Chuan-Shun,Shi, Xue-Fa,Kao, Shuh-Ji,et al. Rare earth elements in fine-grained sediments of major rivers from the high-standing island of Taiwan[J]. JOURNAL OF ASIAN EARTH SCIENCES,2013,69:39-47. |
APA | Li, Chuan-Shun.,Shi, Xue-Fa.,Kao, Shuh-Ji.,Liu, Yan-Guang.,Lyu, Hua-Hua.,...&Qiao, Shu-Qing.(2013).Rare earth elements in fine-grained sediments of major rivers from the high-standing island of Taiwan.JOURNAL OF ASIAN EARTH SCIENCES,69,39-47. |
MLA | Li, Chuan-Shun,et al."Rare earth elements in fine-grained sediments of major rivers from the high-standing island of Taiwan".JOURNAL OF ASIAN EARTH SCIENCES 69(2013):39-47. |
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