ZHU Aimei, LIU Jihua, ZHANG Hui, BAI Yazhi, CUI Jingjing, LIU Shengfa. DISTRIBUTION PATTERN OF REES IN THE INNER-SHELF MUD AREA OF EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 1-10. DOI: 10.3724/SP.J.1140.2012.01001
Citation: ZHU Aimei, LIU Jihua, ZHANG Hui, BAI Yazhi, CUI Jingjing, LIU Shengfa. DISTRIBUTION PATTERN OF REES IN THE INNER-SHELF MUD AREA OF EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 1-10. DOI: 10.3724/SP.J.1140.2012.01001
shu

DISTRIBUTION PATTERN OF REES IN THE INNER-SHELF MUD AREA OF EAST CHINA SEA

  • First Institute of Oceanography, State Oceanic Administration, Key Laboratory of Marine Sedimentology and Environmental Geology, State Oceanic Administration, Qingdao, 266061

More Information
  • Received Date: July 09, 2011
  • Revised Date: August 08, 2011
    Graphical Abstract
    • Abstract
  • Thirty surface samples were collected from the inner-shelf mud areas of the East China Sea. The compositions of rare earth element(REEs), major and minor elements, TOC, CaCO3 and grain size were analyzed for bulk samples. With the results, we discussed in this paper the factors controlling the distribution of the REEs. Results show that the contents of ΣREEs in the inner shelf mud deposits of the East China Sea range from 182.8~221 μg/g with an average of 206.5 μg/g, significantly higher than that in the loess, Yellow River and Yarlung Tsangbo River sediments, but similar to that of the Yangtze River and Oujiang River sediments. Chondrite-normalized REE patterns and (La/Yb)N ratios show that light REE (LREE) are enriched relative to heavy REE (HREE) in sediments with a very strong negative δEu value. Upper continental curst-normalized REE patterns show that the REE of the mud deposits have little fractionation with the UCC and a tetrad pattern of REE were observed in the mud sediments. The weak correlation between REEs and grain size, TOC, CaCO3 indicate that those factors are not critical to the distribution of REEs. The elements ratios and the UCC-normalized pattern of REE suggest that the sediments in the study area are mainly from the Yangtze and Oujiang Rivers.
    • FullText(HTML)
    • References (31)
  • [1]
    赵一阳,鄢明才,李安春, 等. 中国近海沿岸泥的地球化学特征及其指示意义[J]. 中国地质, 2002, 29(2):181-185.

    [ZHAO Yiyang,YAN Mingcai,Li Anchun,et al,Geochemistry of muds along the coast of china and their significance[J]. Geology in China. 2002, 29(2):181-185.]
    [2]
    石学法, 刘升发,乔淑卿, 等. 东海闽浙沿岸泥质区沉积特征与古环境记录[J]. 海洋地质与第四纪地质, 2010, 30(4):19-30.

    [SHI Xuefa,LIU Shengfa,QIAO Shuqing, et al,Depositional features ang palaeoenvironmental records of the mud deposits in min-zhe coastal mud area, east china sea[J]. Maine Geology and Quaternary Geology 2010, 30(4):19-30.]
    [3]
    肖尚斌,李安春,刘卫国,等. 闽浙沿岸泥质沉积的物源分析[J]. 自然科学进展, 2009, 19(2):185-191.

    [XIAO Shangbin,LI Anchun,LIU Weiguo, et al. Sediment provenance analysis in the Min-Zhe mud area[J]. Progress in Natural Science, 2009, 19(2):185-191.]
    [4]
    肖尚斌,李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1):122-129.

    [XIAO Shangbin,LI Anchun. A study on environmentally sensitive grain-size population in inner shelf of the East China Sea[J].Acta Sedimentologica Sinica. 2005, 23(1):122-129.]
    [5]
    郭志刚, 杨作升, 陈致林,等. 东海陆架泥质区沉积有机质的物源分析[J]. 地球化学, 2001, 30(5):416-424.

    [GUO Zhigang,YANG Zuosheng,CHEN Zhilin, et al,Source of sedimentary organic matter in the mud areas of the East China Sea shelf[J]. Geochimica,2001, 30(5):416-424.]
    [6]
    郭志刚, 杨作升,曲艳慧,等. 东海陆架泥质区沉积地球化学比较研究[J]. 沉积学报, 2000, 18(2):284-289.

    [GUO Zhigang,YANG Zuosheng,QU Yanhui, et al, Study on comparison sedimentary geochemistry of mud area on East China Sea Continental Shelf[J].Acta Sedimentologica Sinica2000, 18(2):284-289.]
    [7]
    刘升发, 石学法, 刘焱光,等. 东海内陆架泥质区沉积速率[J]. 海洋地质与第四纪地质, 2009, 29(6):1-7.

    [LIU Shengfa,SHI Xuefa,LIU Yanguang, et al,Sedimention rate of mud area in the East China Sea inner Continental shelf[J]. Marine Geology and Quaternary Geology. 2009, 29(6):1-7.]
    [8] 郭志刚,杨作升,雷坤,等. 东海陆架北部泥质区沉积动力过程的季节性变化[J]. 青岛海洋大学学报(自然科学版), 1999, (3):507-513.[GUO Zhigang,YANG Zuosheng,LEI Kun, et al.Seasonal variation of the sedimentary dynamic processes for the mud area in the Northern East China Sea[J].Journal of Ocean University of Qingdao. 1999, (3):507-513.]
    [9]
    孟庆勇,李安春,徐方建,等. 东海内陆架EC2005孔沉积物磁化率与粒度组分的相关性研究[J]. 科技导报, 2009, 27(10):32-36.

    [MENG Qingyong,LI Anchun,XU Fangjian, et al, Correlation between the grain size distribution and magnetic susceptibility of marine sediment core in the inner shelf of the East China Sea[J]. Science & Technology Review. 2009, 27(10):32-36.]
    [10]
    王可,郑洪波,Maarten P,等. 东海内陆架泥质沉积反映的古环境演化[J]. 海洋地质与第四纪地质, 2008, 28(4):1-10.

    [WANG Ke,ZHENG Hongbo,et al.High resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf[J]. Marine Geology and Quaternary Geology. 2008, 28(4):1-10.]
    [11]
    肖尚斌,李安春,陈木宏,等. 近8ka东亚冬季风变化的东海内陆架泥质沉积记录[J]. 地球科学-中国地质大学学报, 2005, 30(5):573-581.

    [XIAO Shangbin,LI Anchun,CHEN Muhong, et al. Recent 8ka mud records of the East Asian Winter Monsoon from the inner shelf of the East China Sea[J].Earth Science-Journal of China University of Geosciences. 2005, 30(5):573-581.]
    [12]
    肖尚斌,李安春,蒋富清,等. 近2ka来东海内陆架的泥质沉积记录及其气候意义[J]. 科学通报, 2004, (21):2233-2238.[XIAO Shangbin,LI Anchun,JIANG Fuqing, et al.Geochemical characteristics of recent 2

    ka mud on the inner shelf of the East China Sea[J].Geochimica, 2004, (21):2233-2238.]
    [13]
    徐方建, 李安春, 徐兆凯, 等. 东海内陆架沉积物稀土元素地球化学特征及物源意义[J]. 中国稀土学报, 2009, 27(4):574-582.

    [XU Fangjian,LI Anchun,XU Zhaokai, et al. Rare earth element geochemistry in inner shelf of the East China Sea and implication for Sediment provenance[J].Journal of the chinese rare earth society. 2009, 27(4):574-582.]
    [14]
    赵泉鸿,翦知湣,张在秀,等. 东海内陆架泥质沉积区全新世古环境变迁:有孔虫证据[J]. 海洋地质与第四纪地质, 2009, 29(2):75-82.

    [ZHAO Quanhong,JIAN Zhimin,ZHANG Zaixiu, et al. Holocene paleoenvironmental changes of the inner shelf mud area of the East China Sea:evidence from foraminiferal faunas[J]. Marine Geology and Quaternary Geology 2009, 29(2):75-82.]
    [15]
    刘升发,石学法,刘焱光,等. 东海内陆架泥质区表层沉积物常量元素地球化学及其地质意义[J]. 海洋科学进展, 2010, 28(1):80-86.

    [LIU Shengfa,SHI Xuefa,LIU Yanguang, et al. Geochemical characteristics and geological significance of major elements in the surface sediments from the inner shelf mud area of the East China Sea[J].Advances in Marine Science. 2010, 28(1):80-86.]
    [16]
    邹建军,石学法,刘季花,等. 48ka以来日本海古生产力和古氧化还原环境变化的地球化学记录[J]. 海洋学报, 2010, 32(4):98-109.

    [ZOU Jianjun,SHI Xuefa,LIU Jihua, et al. The geochemical records of paleoproductivity and paleoredox in the sea of Japan since 48 ka[J]. Acta Oceanologica Sinica. 2010, 32(4):98-109.]
    [17]
    Taylor S R,McLennan S M. The continental crust:Its composition and evolution[M]. 1 edn Palo Alto,CA:Blackwell Scientific Publisher, 1985.
    [18]
    Liu C Q, Masuda A, Okada A, et al. A geochemical study of loess and desert sand in northern China:Implications for continental crust weathering and composition[J]. Chemical Geology, 1993, 106(3-4):359-374.
    [19]
    Gaillardeta J, Dupre B,Allegre C J. Geochemistry of large river suspended sediments:Silicate weathering or recycling tracer?[J]. Geochimica et Cosmochimica Acta, 1999, 63(23-24):4037-4051.
    [20]
    Zhang C,Wang L. Multi-element geochemistry of sediments from the Pearl River system, China[J]. Applied Geochemistry, 2001, 16(9-10):1251-1259.
    [21]
    Li C, Kang S, Zhang Q, et al. Rare earth elements in the surface sediments of the Yarlung Tsangbo (Upper Brahmaputra River) sediments, southern Tibetan Plateau[J]. Quaternary International, 2009, 208(1-2):151-157.
    [22]
    Sun S S,McDonough W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313-345.
    [23]
    宋云华,沈丽璞,王贤觉. 某些岩石风化壳中稀土元素的初步探讨[J]. 科学通报, 1987, 32(9):695-695.

    [SONG Yunhua,SHEN Lipu,WANG Xianjue. A preliminary study for REEs in the weathering crust of some kinds of rocks[J]. Chinese Science Bulletin, 1987, 32(9):695-695.]
    [24]
    Masuda A, Kawakami O, Dohmoto Y, et al. Lanthanide tetrad effects in nature:two mutually opposite types, W and M[J]. Geochemical Journal, 1987, 21:119-124.
    [25]
    Nesbitt H,Young G. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature, 1982, 299:715-717.
    [26]
    Gu X, Liu J, Zheng M, et al. Provenance and tectonic setting of the Proterozoic turbidites in Hunan, South China:Geochemical Evidence[J]. Journal of Sedimentary Research, 2002, 72(3):393-407.
    [27]
    苗卫良,邵磊, 庞雄,等. 南海北部渐新世以来的稀土元素地球化学特征及其意义[J]. 海洋地质与第四纪地质, 2008, 28(2):71-78.

    [MIAO Weiliang,SHAO Lei,PANG Xiong et al.Ree geochemical characteristics in the Northern South China Sea since the oligocene[J]. Marine Geology and Quaternary Geology. 2008, 28(2):71-78.]
    [28]
    蒋富清,周晓静,李安春,等. ΔEu_N-ΣREEs图解定量区分长江和黄河沉积物[J]. 中国科学D辑, 2008, 38(11):1460-1468.

    [JIANG Fuqing,ZHOU Xiaojing,LI Anchun, et al. Quantitatively distinguishing sediments from the Yangtze River and the Yellow River using δEuN-ΣREEs plot[J]. Science in China(Series D). 2008, 38(11):1460-1468.]
    [29]
    高爱国,陈志华,刘焱光,等. 楚科奇海表层沉积物的稀土元素地球化学特征[J]. 中国科学D辑, 2003, 33(2):148-154.

    [GAO Aiguo,Chen Zhihua, LIU Yanguang, et al. REE geochemistry of surface sediments in the Chukchi Sea[J]. Science in China(Series D). 2003, 33(2):148-154.]
    [30]
    Bhatia M R,Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 1986, 92(2):181-193.
    [31]
    Cullers R L. The controls on the major and trace element variation of shales, siltstones, and sandstones of Pennsylvanian-Permian age from uplifted continental blocks in Colorado to platform sediment in Kansas, USA[J]. Geochimica et Cosmochimica Acta, 1994, 58(22):4955-4972.
    • Related Articles

Catalog

    Get Citation
    PDF
    XML
    Article views (2159) PDF downloads (11) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return