南海西南海域表层沉积物微量和稀土元素地球化学特征及其意义

蔡观强, 邱燕, 彭学超, 钟和贤

蔡观强, 邱燕, 彭学超, 钟和贤. 南海西南海域表层沉积物微量和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, 2010, 30(5): 53-62. DOI: 10.3724/SP.J.1140.2010.05053
引用本文: 蔡观强, 邱燕, 彭学超, 钟和贤. 南海西南海域表层沉积物微量和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, 2010, 30(5): 53-62. DOI: 10.3724/SP.J.1140.2010.05053
CAI Guanqiang, QIU Yan, PENG Xuechao, ZHONG Hexian. THE GEOCHEMICAL CHARACTERISTICS OF TRACE ELEMENTS AND REES IN SURFICIAL SEDIMENTS OF THE SOUTHWESTERN SOUTH CHINA SEA AND THEIR IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2010, 30(5): 53-62. DOI: 10.3724/SP.J.1140.2010.05053
Citation: CAI Guanqiang, QIU Yan, PENG Xuechao, ZHONG Hexian. THE GEOCHEMICAL CHARACTERISTICS OF TRACE ELEMENTS AND REES IN SURFICIAL SEDIMENTS OF THE SOUTHWESTERN SOUTH CHINA SEA AND THEIR IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2010, 30(5): 53-62. DOI: 10.3724/SP.J.1140.2010.05053

南海西南海域表层沉积物微量和稀土元素地球化学特征及其意义

基金项目: 

国家自然科学青年基金项目(41006025)

中国科学院海洋地质与环境重点实验室开放基金项目(MGE2010KG01)

详细信息
    作者简介:

    蔡观强(1981-),男,博士,主要从事海洋沉积地球化学研究,E-mail:caiguanqiang@sina.com

  • 中图分类号: P736.4

THE GEOCHEMICAL CHARACTERISTICS OF TRACE ELEMENTS AND REES IN SURFICIAL SEDIMENTS OF THE SOUTHWESTERN SOUTH CHINA SEA AND THEIR IMPLICATIONS

  • 摘要: 分析了南海西南海域表层沉积物的微量元素和稀土元素组成,结果表明,这些沉积物与大陆上地壳相比,具有相对低的Zr、Sc、V、Nb、Hf、Th、REEs含量,而Co、Cu、Ni、Ta、Rb、Cs、Sr、Ba的含量稍高;深海区表层沉积物比陆坡区具有较高的Co、Zr、Sc、V、Nb、Hf、Ta、Th和REEs,陆坡区表层沉积物相对高的生物碎屑组分对这些元素起到了一定程度的稀释作用。因子分析和相关分析显示绝大部分微量元素和稀土元素主要受陆源组分的控制,Th、Cr、Co、Sc、Nb、Zr、Hf和REEs等不活动元素之间的比值特征,并没有受到风化作用、海流搬运作用和海洋自生组分稀释作用的影响,较好地保存了源岩的化学组成特征。因此,南海西南海域表层沉积物的La/Sc、Th/Sc、Th/Cr、Th/Co比值和稀土配分曲线特征,指示这些沉积物的源岩具有陆壳成分的特点,以长英质岩石为主,缺乏深源的基性和超基性岩,火山碎屑物质成分很低,其源区主要为南海西部的印支大陆。陆架区和深海区表层沉积物具有十分相近的微量元素和稀土元素组成特征,指示它们的碎屑物质来源较为相同。
    Abstract: This paper presents the trace elements and REEs composition of the surficial sediments from the southwestern South China Sea (SCS). The results show that the samples have relatively low Zr, Sc, V, Nb, Hf, Th, REEs contents and high Co, Cu, Ni, Ta, Rb, Cs, Sr, Ba contents, compared with the upper continental crust (UCC). The sediments from marine basins have higher Co, Zr, Sc, V, Nb, Hf, Ta, Th and REEs abundances than those from the continental slope. Factor and correlation analyses indicate that most of these elements are land-derived.The immobile elements such as Th, Cr, Co, Sc, Nb, Zr, Hf and REEs are indicators of source rocks.There shows no influences from weathering, transportation and diluting effect of biologic materials.The high La/Sc, Th/Sc, Th/Cr, Th/Co ratios and UCC-like rare earth elements distribution patterns characterized by high ΣLREE/ΣHREE ratios and low δEu values suggest that the source of the studied sediments are mainly from continental crust with felsic rocks as the majority, but the contribution of basic/ultrabasic rocks is ignorable and the volcanic clast content in the sediments is also very low. With reference to the geography of the studied areas, the geochemistry of surficial sediments from the southwestern SCS indicates that the materials are mainly from neighbour continents, probably the Indo-China block.Both the continental slope and marine basins show a common provenance according to their similarity in trace and rare earth elements compositions.
  • [1]

    WANG L J, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene:high-resolution sediment records from the South China Sea[J]. Marine Geology, 1999, 156:245-284.

    [2] 钱建兴. 晚第四纪以来南海古海洋学研究[M]. 北京:科学出版社, 1999:1-167.[QIAN Jianxing.A Study of Paleoceanography in the South China Sea During Late Quaternary[M]. Beijing:Science Press, 1999.]
    [3] 翦知湣, 王吉良, 成鑫荣, 等. 南海北部晚新生代氧同位素地层学[J].中国科学D辑,2001,31(10):800-807.

    [JIAN Zhimin, WANG Jiliang, CHENG Xinrong, et al. Oxygen isotope stratigraphy and events in the northern South China Sea during the last 6 million years[J]. Science in China (Series D), 2001, 31(10):800-807.]

    [4] 汪品先, 翦知湣, 赵泉鸿, 等. 南海演变与季风历史的深海证据[J]. 科学通报, 2003, 48(21):2228-2239.

    [WANG Pinxian, JIAN Zhimin, ZHAO Quanhong, et al. Evolution of the South China Sea and monsoon history revealed in deep sea records[J]. Chinese Science Bulletin, 2003, 48(21):2228-2239.]

    [5]

    Wei G J, Liu Y, Li X H, et al. High-resolution elemental records from the South China Sea and their paleoproductivity implications[J]. Paleoceanography, 2003a, 18:1054-1065.

    [6] 汪品先. 十五万年来的南海[M]. 上海:同济大学出版社, 1995.[WANG Pinxian. South China Sea Since 150000 Years[M]. Shanghai:Publishing House of Tongji University, 1995.]
    [7]

    Wang P X. Response of western Pacific marginal seas to glacial cycles:Paleoceanographic and sedimentological features[J]. Marine Geo1ogy, 1999, 156:5-39.

    [8]

    Wei, G J, Shao L, Liu Y, et al. Climatic impact on Al, K, Sc and Ti in marine sediments:Evidence from ODP Site 1144, South China Sea. Geochemical Journal, 2003b, 37:593-602.

    [9]

    Clift P D, Sun Z.The sedimentary and tectonic evolution of the Yinggehai Song Hong Basin and the southern Hainan margin, South China Sea; implications for Tibetan uplift and monsoon intensification[J]. Journal of Geophysical Research 111,2006,B06405. doi:10.1029/2005 JB004048.

    [10] 刘志飞, 赵玉龙, 李建如, 等. 南海西部越南岸外晚第四纪粘土矿物记录:物源分析与东亚季风演化[J]. 中国科学D辑, 2007, 37(9):1176-1184.

    [LIU Zhifei, ZHAO Yulong, LI Jianru, et al. Late Quaternary clay minerals off Middle Vietnam in the western South China Sea:Implications for source analysis and East Asian monsoon evolution[J]. Science in China (Series D), 2007, 37(9):1176-1184.]

    [11]

    McLennan S M. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes[J]. Reviews in Mineralogy, 1989, 21:170-199.

    [12]

    Cullers R L. The controls on the major and trace element variation of shales, siltstones and sandstones of Pennsylvanian-Permian age, from uplifted continental block in Colorado to platform sediment in Kansas, USA[J]. Geochimica et Cosmochimica Acta, 1994, 55:4955-4972.

    [13] 金秉福, 林振宏. 海洋沉积环境和物源的元素地球化学记录释读[J]. 海洋科学进展, 2003, 21(1):99-106.

    [JIN Bingfu, LIN Zhenhong. Interpretation of element geochemical records of marine sedimentary environment and provenance[J]. Advance in Marine Science, 2003, 21(1):99-106.]

    [14] 刘季花, 石学法, 陈丽蓉,等. 东太平洋沉积物中粘土组分的REEs和εNd——粘土来源的证据[J]. 中国科学D辑, 2004, 34(6):552-561.

    [LIU Jihua, SHI Xuefa, CHEN Li-rong, et al. REE and εNd of clay fractions in sediments from the eastern Pacific Ocean:Evidence for clay sources[J]. Science in China (Series D), 2004, 34(6):552-561.]

    [15] 邵磊, 李献华, 韦刚健, 等. 南海陆坡高速堆积体的物质来源[J]. 中国科学D辑, 2001, 31(10):828-833.

    [SHAO Lei, LI Xianhua, WEI Gangjian, et al. Material source of high-speed congeries in South China Sea[J]. Science in China (Series D), 2001, 31(10):828-833.]

    [16]

    Li X H, Wei G J, Liu Y, et al. Geochemical and Nd isotopic variations in sediments of the South China Sea:a response to Cenozoic tectonism in SE Asia[J]. Earth and Planetary Science Letters, 2003, 211:207-220.

    [17]

    Tamburini F, Adatte T, F llmi K, et al. Investigating the history of East Asian monsoon and climate during the last glacial interglacial period (0~140000 years):mineralogy and geochemistry of ODP Sites 1143 and 1144, South China Sea[J]. Marine Geology, 2003, 201:147-168.

    [18]

    Boulay S, Colin C, Trentesaux A, et al. Mineralogy and sedimentology of Pleistocene sediment in the South China Sea (ODP Site 1144)[C]. In:Prell W L, Wang P, Blum P, et al, eds. Proc ODP Sci Res, 2003, 184:1-21.

    [19]

    Wehausen R, Brumsack H J. Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments[J].Earth Planet Sci.Lett., 2002, 201:621-636.

    [20] 乔培军, 邵磊, 杨守业. 南海西南部晚更新世以来元素地球化学特征的古环境意义[J]. 海洋地质与第四纪地质, 2006, 26(4):59-65.

    [QIAO Peijun, SHAO Lei, YANG Shouye. The paleoenvironmental significance of the character of the element geochemistry in the southwestern South China Sea since late Pleistocene[J]. Marine Geology and Quaternary Geology, 2006, 26(4):59-65.]

    [21] 朱赖民, 高志友, 尹观, 等.南海表层沉积物的稀土和微量元素的丰度及其空间变化[J].岩石学报, 2007, 23(11):2963-2980.

    [ZHU Laimin, GAO Zhiyou, YIN Guan,et al. Content and spatial change of rare earth element and trace element of surficial sediment in the South China Sea[J]. Acta Petrologica Sinica, 23(11):2963-2980.]

    [22]

    Rudnick R L,Gao S. Composition of the Continental Crust[C]. Oxford:the Oxford Press, Treatise On Geochemistry, Vol. 3, 2003.

    [23]

    Taylor S R,McLennan S M. The Continental Crust:Its composition and Evolution[M]. Blackwell, Oxford, 1985.

    [24]

    Holser W T. Evaluation of the application of rare-earth elements to paleoceanography[J]. Paleoceanography, Paleaoclimatology, Paleaoecology, 1997, 132:309-323.

    [25]

    Nessbitt H W, Markovics G, Price R C. Chemical processes affecting alkalis and alkaline earths during continental weathering[J]. Geochimica et Cosmochimica Acta, 1980, 6:887-898.

    [26]

    Nesbitt H W, Markovics G. Weathering of granodioritic crust, long-term storage of elements in weathering profiles, and petrogenesis of siliciclastic sediments[J]. Geochim. Cosmochim. Acta, 1997, 61(8):1653-1670.

    [27]

    Crichton J G, Condie K C. Trace elements as source indicators in cratonic sediments:a case study from the early Proterozoic Libby Creek Group, southeastern Wyoming[J]. The Journal of Geology, 1993, 101:319-332.

    [28]

    Condie K C, Dengate J, Cullers R L. Behavior of rare earth elements in a paleoweathering profile on granodiorite in the Front Range, Colorado, USA[J]. Geochim. Cosmochim. Acta, 1995, 59:279-294.

    [29]

    Sharma A, Rajamani V. Major element, REE and other trace element behavior in amphibolite weathering under semiarid conditions in Southern India[J]. Journal of Geology, 2000, 108:487-496.

    [30]

    McLennan S M, Taylor S R. Sedimentary rocks and crustal evolution:tectonic setting and secular trend[J]. Journal of Geology, 1991, 99:1-21.

    [31]

    McLennan S M, Hemming S, Mcdaniel D K, et al. Geochemical approaches to sedimentation, provenance and tectonics[C]//In Jonhanson M J et al eds.Processes controlling the composition of clastic sediments. Boulder:Geological Society of America Special Paper, 1993, 284:21-40.

    [32] 鄢全树, 石学法, 王昆山, 等. 南海新生代碱性玄武岩主量、微量元素及Sr-Nd-Pb同位素研究[J]. 中国科学D辑:地球科学, 2008, 38(1):56-71.

    [YAN Quanshu, SHI Xuefa, WANG Kunshan, et al. Major element, trace element, and Sr, Nd and Pb iso-tope studies of Cenozoic basalts from the South China Sea[J]. Science in China (Series D), 2008, 38(1):56-71.]

    [33]

    Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic controls[J]. Sedimemtary Geology, 1985, 45:97-113.

    [34]

    Cullers R L. The geochemistry of shales, siltstones and sandstones of Pennsylvanian-Permian age, Colorado, USA:implications for provenance and metamorphic studies[J]. Lithos, 2000, 51:181-203.

    [35]

    Condie K C. Chemical composition and evolution of the upper continental crust:contrasting results from surface samples and shales[J]. Chemical Geology, 1993, 104:1-37.

    [36] 刘志飞,Colin C, Trentesaux A, 等. 青藏高原东部和泥公河盆地晚第四纪风化剥蚀与东亚季风演化在南海中的记录[J]. 矿物岩石地球化学通报, 2005, 24(1):30-38.

    [LIU Zhifei, Colin C, Trentesaux A, et al. Late Quaternary weathering and erosion of the eastern Tibetan plateau and the Mekong basin and east Asian monsoon evolution recorded by the sediments from the South China Sea[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2005, 24(1):30-38.]

计量
  • 文章访问数:  2452
  • HTML全文浏览量:  444
  • PDF下载量:  98
  • 被引次数: 0
出版历程
  • 收稿日期:  2010-01-18
  • 修回日期:  2010-06-29

目录

    /

    返回文章
    返回