Geochemical character and material source of sediments in the eastern Philippine Sea | |
Xu ZhaoKai1,2,3,4; Li AnChun1; Jiang FuQing1; Xu FangJian1,4 | |
发表期刊 | CHINESE SCIENCE BULLETIN |
ISSN | 1001-6538 |
2008-03-01 | |
卷号 | 53期号:6页码:923-931 |
关键词 | Sediment Grain-size Rare Earth Elements Discriminant Function Elemental Occurrence Phase Material Source Eastern Philippine Sea |
产权排序 | Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm;Kunsan Natl Univ, Dept Oceanog; Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Deva;Chinese Acad Sci, Grad Univ, |
通讯作者 | Li, AC, Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China |
作者部门 | 生物资源实验室 |
英文摘要 | Based upon analyses of grain-size, rare earth element (REE) compositions, elemental occurrence phases of REE, and U-series isotopic dating, the sediment characteristics and material sources of the study area were examined for the recently formed deep-sea clays in the eastern Philippine Sea. The analytical results are summarized as follows. (1) Low accumulation rate, poor sorting and roundness, and high contents of grains coarser than fine silt indicate relatively low sediment input, with localized material source without long distance transport. (2) The REE Contents are relatively high. Shale-normalized patterns of REE indicate weak enrichment in heavy REE (HREE), Ce-passive anomaly, and Eu-positive anomaly. (3) Elemental occurrence phases of REE between the sediments with and without crust are similar. REE mainly concentrate in residual phase and then in ferromanganese oxide phase. The light REE (LREE) enrichment, Ce-positive anomaly, and Eu-positive anomaly occur in residual phase. Ferromanganese oxide phase shows the characteristics of relatively high HREE content and Ce-passive anomaly. (4) There are differences in each above mentioned aspect between the sediments with and without ferromanganese crust. (5) Synthesizing the above characteristics and source discriminant analysis, the study sediments are deduced to mainly result from the alteration of local and nearby volcanic materials. Continental materials transported by wind and/or river (ocean) flows also have minor contributions. |
文章类型 | Article |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | RARE-EARTH-ELEMENTS ; NORTH PACIFIC ; OCEAN ; CRUST ; ASIA |
研究领域[WOS] | Science & Technology - Other Topics |
WOS记录号 | WOS:000254360500016 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.yic.ac.cn/handle/133337/3505 |
专题 | 海岸带生物学与生物资源利用重点实验室_海岸带生物学与生物资源保护实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Kunsan Natl Univ, Dept Oceanog, Kunsan 573701, South Korea 3.Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China 4.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Xu ZhaoKai,Li AnChun,Jiang FuQing,et al. Geochemical character and material source of sediments in the eastern Philippine Sea[J]. CHINESE SCIENCE BULLETIN,2008,53(6):923-931. |
APA | Xu ZhaoKai,Li AnChun,Jiang FuQing,&Xu FangJian.(2008).Geochemical character and material source of sediments in the eastern Philippine Sea.CHINESE SCIENCE BULLETIN,53(6),923-931. |
MLA | Xu ZhaoKai,et al."Geochemical character and material source of sediments in the eastern Philippine Sea".CHINESE SCIENCE BULLETIN 53.6(2008):923-931. |
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