| Elemental and Sr-Nd isotopic compositional disparity of riverine sediments around the Yellow Sea: Constraints from grain-size and chemical partitioning | |
Lim, Dhongil1,2; Jung, Hoisoo3; Xu, Zhaokai1,4,5; Jeong, Kapsik3; Li, Tiegang4
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| 2015-12-01 | |
| 发表期刊 | APPLIED GEOCHEMISTRY
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| 卷号 | 63期号:2015页码:272-281 |
| 文章类型 | Article |
| 摘要 | To obtain a better understanding of the source compositions of the river sediments around the Yellow Sea and their relationship with source rocks, elements and strontium-neodymium (Sr-Nd) isotopes of different grain-sizes (silt and clay populations) and chemical (labile and residual phases) fractionations in riverine sediments were studied extensively. These results clearly revealed a systematic compositional disparity between Korean river (KR) and Chinese river (CR) sediments, especially in the residual (detrital) fraction. The geochemical dissimilarity between these might reflect inherited signatures of their source rocks but with minor control from chemical weathering. In particular, the remarkable enrichment of some elements (iron (Fe) and magnesium (Mg)) and the behavior of large ion lithophile elements (e.g., barium (Ba), potassium (K) and Sr) during weathering as well as less-radiogenic Sr isotopic compositions implies that CR sediments might be weathering products of relatively more mafic rocks, with abundant ferromagnesian and plagioclase feldspar minerals, compared with KR sediments derived from silicic granites with relatively higher quartz and potassium feldspar contents. This different petrological rationale is clearly evident in an A-CN-K diagram, which estimated the source rock of CR sediments as granodioritic, a composition that reflects accurately the average composition of weathered continental crust in China. The recognition of such geochemical systematics in two river sediments, especially in grain-size and chemically partitioned data, may contribute to the establishment of provenance tracers for the Yellow Sea and East China Sea sediments with multi-sources as well the dust deposition in the western Pacific. (C) 2015 Elsevier Ltd. All rights reserved. |
| 关键词 | Elemental Compositions Sr-nd Isotopes Sediment Origin Silicate Weathering Yellow Sea |
| DOI | 10.1016/j.apgeochem.2015.09.018 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000366219800023 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/86627 |
| 专题 | 海洋地质与环境重点实验室 |
| 作者单位 | 1.Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea 2.Univ Sci & Technol, Marine Environm Chem & Biol, Daejeon 305350, Peoples R China 3.Korea Inst Ocean Sci & Technol, Marine Environm & Conservat Res Dept, Seoul 425600, South Korea 4.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 5.Qingdao Natl Lab Marine Sci & Technol, Funct Lab Marine Geol & Environm, Qingdao 266061, Peoples R China |
| 推荐引用方式 GB/T 7714 | Lim, Dhongil,Jung, Hoisoo,Xu, Zhaokai,et al. Elemental and Sr-Nd isotopic compositional disparity of riverine sediments around the Yellow Sea: Constraints from grain-size and chemical partitioning[J]. APPLIED GEOCHEMISTRY,2015,63(2015):272-281. |
| APA | Lim, Dhongil,Jung, Hoisoo,Xu, Zhaokai,Jeong, Kapsik,&Li, Tiegang.(2015).Elemental and Sr-Nd isotopic compositional disparity of riverine sediments around the Yellow Sea: Constraints from grain-size and chemical partitioning.APPLIED GEOCHEMISTRY,63(2015),272-281. |
| MLA | Lim, Dhongil,et al."Elemental and Sr-Nd isotopic compositional disparity of riverine sediments around the Yellow Sea: Constraints from grain-size and chemical partitioning".APPLIED GEOCHEMISTRY 63.2015(2015):272-281. |
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| Elemental and Sr-Nd （1543KB） | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 | |
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