2007 Vol. 27, No. 6
Article Contents

CHEN Hong, LIU Jian, WANG Hong-bin. GEOCHEMICAL CHARACTERISTICS AND GEOLOGICAL SIGNIFICANCE OF MAJOR ELEMENTS IN SURFACE SEDIMENTS IN QIONGDONGNAN AREA[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 39-45.
Citation: CHEN Hong, LIU Jian, WANG Hong-bin. GEOCHEMICAL CHARACTERISTICS AND GEOLOGICAL SIGNIFICANCE OF MAJOR ELEMENTS IN SURFACE SEDIMENTS IN QIONGDONGNAN AREA[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 39-45.

GEOCHEMICAL CHARACTERISTICS AND GEOLOGICAL SIGNIFICANCE OF MAJOR ELEMENTS IN SURFACE SEDIMENTS IN QIONGDONGNAN AREA

  • Geochemical characteristics and geological significance of surface sediments from the Qiongdongnan area are studied. 88 sediment samples have been analyzed for their major element contents. SiO2 is of the highest content in the area, with its mean content up to 41.15%. CaO following SiO2, its mean content is 15.66%.Terrestrial clasts in the area were mainly carried by Honghe River from Western Yunnan Plateau. Factor analysis shows that SiO2,Al2O3,Fe2O3,MgO,K2O and TiO2 originate from terrestrial source and CaO,CaCO3 and LOSS are mainly derived from marine calcicolous livings. Meanwhile, P2O5 and Corg mainly come from mixed terrestrial matrials and marine livings and Na2O and MnO are mostly products of marine chemistry or volcanism. However, the components of terrestrial clastic and biological materials are primary factors that control the chemical compositions of sediments in the study area.
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  • [1] 张启明,郝芳.莺-琼盆地演化与含油气系统[J].中国科学D辑,1997,27(2):149-154.

    Google Scholar

    [ZHANG Qi-ming,HAO Fang. Evolution of Ying-Qiong Basin and oil-gas system[J]. Science in China(Series D),1997,27(2):149-154.]

    Google Scholar

    [2] 魏魁生,崔旱云,叶淑芬,等.琼东南盆地高精度层序地层学研究[J].地球科学-中国地质大学学报,2001,26(1):59-66.

    Google Scholar

    [WEI Kui-sheng,CUI Han-yun,YE Shu-fen,et al. High-precision sequence stratigraphy in Qiongdongnan Basin[J]. Earth Science-Journal of China University of Geosciences,2001,26(1):59-66.]

    Google Scholar

    [3] 何家雄,李强,陈伟煌,等.琼东南盆地油气成因类型及近期天然气勘探方向探讨[J].海洋石油,2002,111:47-58.[HE Jia-xiong,LI Qiang,CHEN Wei-huang,et al. Oil/gas mechanism type and gas exploratory direction in southeast Hainan Basin[J].Marine Petroleum,2002

    Google Scholar

    ,111:47-58.]

    Google Scholar

    [4] 陈多福,李绪宣,夏斌.南海琼东南盆地天然气水合物稳定域分布特征及资源预测[J].地球物理学报,2004,47(3):483-489.

    Google Scholar

    [CHEN Duo-fu,LI Xu-xuan,XIA Bin,et al. Distribution of gas hydrate stable zones and resource prediction in the Qiongdongnan Basin of the South China Sea[J]. Chinese J. Geophys.,2004,47(3):483-489.]

    Google Scholar

    [5] 古森昌,陈忠,颜文,等.南沙海槽区表层沉积物的地球化学特征[J].海洋地质与第四纪地质,2001,21(2):43-47.

    Google Scholar

    [GU Sen-chang,CHEN Zhong,YAN Wen,et al. Geochemical characteristics and sedimentary environment of surface sediments of south Nansha Trough and adjacent sea areas[J].Marine Geology and Quaternary Geology,2001, 21(2):43-47.]

    Google Scholar

    [6] 中国科学院南沙综合科学考察队. 南沙群岛及其临近海区第四纪沉积地质学[M]. 湖北:科学技术出版社,1993:107-133.[Nansha Scientific Research Team of Chinese Academy of Sciences. Quaternary Sedimentary Geology in Nansha Islands and Adjacent Sea Areas[M]. Hubei:Science and Technology Press,1993:107

    Google Scholar

    -133.]

    Google Scholar

    [7] 赵一阳,鄢明才.中国浅海沉积物地球化学[M]. 北京:科学出版社,1994.[ZHAO Yi-yang, YAN Ming-cai. Geochemistry of Shallow-Sea Sediments in China[M]. Beijing:Science Press,1994.]

    Google Scholar

    [8] 许德如,梁新权,陈广浩,等.海南岛中元古代花岗岩地球化学及成因研究[J].大地构造与成矿学,2001,25(4):420-433.

    Google Scholar

    [XU De-ru,LIANG Xin-quan,CHEN Guang-hao,et al.Research on the geochemistry and genesis of mesoproterozoic granites on Hainan Island[J].Geotectonica et Metallogenia,2001,25(4):420-433.]

    Google Scholar

    [9] 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,2003b,18(2):1054-1065.

    Google Scholar

    [10] Murray R W,Knowlton C,Leinen M,et al. Export production and terrigenous matter in the Central Equatorial Pacific Ocean during interglacial oxygen isotope stage 11[J]. Glob.Planet. Change,2000,24:59-78.

    Google Scholar

    [11] 韦刚健,刘颖,李献华,等. 南海沉积物中过剩铝问题的探讨[J].矿物岩石地球化学通报,2003,22(1):23-25.

    Google Scholar

    [WEI Gang-jian,LIU Ying,LI Xian-hua,et al. Excess Al in the sediments from South China Sea[J].Bulletin of Mineralogy Petrology and Geochemistry,2003,22(1):23-25.]

    Google Scholar

    [12] Murray R W,Leinen M. Scavenged excess aluminum and its relationship to bulk titanium in biogenic sediment from the central equatorial Pacific Ocean[J]. Geochim. Cosmochim.Acta,1996,60(20):3869-3878.

    Google Scholar

    [13] 王国芝,王成善,刘登忠,等.滇西高原第四纪以来的隆升和剥蚀[J].海洋地质与第四纪地质,1999,19(4):67-74.

    Google Scholar

    [WANG Guo-zhi,WANG Cheng-shan,LIU Deng-zhong,et al.Uplift and denudation of the Western Yunnan Plateau in Quaternary[J]. Marine Geology and Quaternary Geology,1999,19(4):67-74.]

    Google Scholar

    [14] 王国芝,王成善,曾允孚,等.滇西高原的隆升与莺歌海盆地的沉积响应[J].沉积学报,2000,18(2):234-240.

    Google Scholar

    [WANG Guo-zhi,WANG Cheng-shan,ZENG Yun-fu,et al. The uplift of the western Yunnan Plateau and the sedimentary response of the Yinggehai Basin[J]. Acta Sedimentologica Sinica,2000,18(2):234-240.]

    Google Scholar

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