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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
2015-12-01
Source PublicationAPPLIED GEOCHEMISTRY
Volume63Issue:2015Pages:272-281
SubtypeArticle
AbstractTo 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.
KeywordElemental Compositions Sr-nd Isotopes Sediment Origin Silicate Weathering Yellow Sea
DOI10.1016/j.apgeochem.2015.09.018
Indexed BySCI
Language英语
WOS IDWOS:000366219800023
Citation statistics
Cited Times:6[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.qdio.ac.cn/handle/337002/86627
Collection海洋地质与环境重点实验室
Affiliation1.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
Recommended Citation
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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