西太平洋采薇海山群基岩特征

韦振权, 邓希光, 朱克超, 姚会强, 杨永, 任江波. 西太平洋采薇海山群基岩特征[J]. 海洋地质前沿, 2017, 33(12): 1-6. doi: 10.16028/j.1009-2722.2017.12001
引用本文: 韦振权, 邓希光, 朱克超, 姚会强, 杨永, 任江波. 西太平洋采薇海山群基岩特征[J]. 海洋地质前沿, 2017, 33(12): 1-6. doi: 10.16028/j.1009-2722.2017.12001
WEI Zhenquan, DENG Xiguang, ZHU Kechao, YAO Huiqiang, YANG Yong, REN Jiangbo. CHARACTERISTIC OF SUBSTRATE ROCKS OF CAIWEI SEAMOUNTS IN THE WEST PACIFIC OCEAN[J]. Marine Geology Frontiers, 2017, 33(12): 1-6. doi: 10.16028/j.1009-2722.2017.12001
Citation: WEI Zhenquan, DENG Xiguang, ZHU Kechao, YAO Huiqiang, YANG Yong, REN Jiangbo. CHARACTERISTIC OF SUBSTRATE ROCKS OF CAIWEI SEAMOUNTS IN THE WEST PACIFIC OCEAN[J]. Marine Geology Frontiers, 2017, 33(12): 1-6. doi: 10.16028/j.1009-2722.2017.12001

西太平洋采薇海山群基岩特征

  • 基金项目:
    国家自然科学基金(41606071); 国际海域资源调查与开发"十二五"课题(DY125-13-R-05,DY125-13-R-01)
详细信息
    作者简介: 韦振权(1978-), 男, 博士, 高级工程师, 主要从事大洋矿产资源与南海油气资源的调查与研究工作.E-mail:wei_zhenquan@163.com
  • 中图分类号: P736.1

CHARACTERISTIC OF SUBSTRATE ROCKS OF CAIWEI SEAMOUNTS IN THE WEST PACIFIC OCEAN

  • 对西太平洋采薇海山群基岩的类型、分布及岩石学特征进行了研究,同时对该海山群玄武岩主量元素和微量元素地球化学特征进行了初步分析。研究结果表明,采薇海山群的基岩类型主要为火山碎屑岩、灰岩、玄武岩和磷块岩;海山群的基岩以火山碎屑岩为主,其次为灰岩和玄武岩,磷块岩相对不发育。镜下鉴定结果显示,火山碎屑岩以玄武质火山角砾岩为主,灰岩主要为泥晶生屑灰岩或亮晶生屑灰岩,磷块岩多由生物碎屑灰岩或火山碎屑岩发生磷酸盐化而形成。采薇海山群玄武岩主量元素特征与夏威夷岛碱性玄武岩类似,属碱性玄武岩;微量元素分析结果显示其具有洋岛和碱性玄武岩特征,反映其形成于碱性洋岛构造环境。

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  • 图 1  麦哲伦海山区构造简图 (据文献[5]修改)

    Figure 1. 

    图 2  采薇海山群浅钻取样获取的各类基岩分布

    Figure 2. 

    图 3  采薇海山群基岩显微照片

    Figure 3. 

    图 4  采薇海山群玄武岩Zr/TiO2—Nb/Y分类 (据文献[17])

    Figure 4. 

    图 5  采薇海山群玄武岩微量元素蛛网图

    Figure 5. 

    图 6  采薇海山群玄武岩Th—Hf—Nb判别图 (据文献[20])

    Figure 6. 

    表 1  采薇海山群玄武岩主量元素含量(%)和微量元素含量(μg/g)

    Table 1.  Major elements(%) and trace elements(μg/g) contents of basalts from Caiwei Seamounts

    样品 MASD07[14] MASD12[15] MASD21[15] MASD23[15] MAD23[16] MAD24[15] MASD27[16] MASD31[16] MASD33[16] MASD39[16]
    SiO2 38.18 45.50 39.83 34.09 39.97 53.75 51.31 48.76 49.58 42.45
    Al2O3 18.39 15.76 13.28 13.16 14.14 7.84 18.03 17.81 16.85 16.03
    Fe2O3 14.85 14.89 15.36 9.53 17.28 17.23 9.94 12.82 13.20 13.86
    MgO 0.06 3.13 1.38 2.46 3.96 1.33 2.31 1.56 2.22 4.13
    CaO 9.68 6.22 9.02 16.44 8.32 3.35 5.79 5.26 6.42 8.73
    Na2O 2.64 3.55 2.60 1.91 2.60 4.46 3.44 3.25 3.54 1.99
    K2O 1.43 1.80 3.61 1.39 1.42 1.94 2.50 2.09 1.73 1.54
    MnO 2.27 0.54 1.90 1.25 0.29 0.27 0.16 0.06 0.17 0.16
    TiO2 3.40 1.85 2.44 2.58 3.17 2.09 2.51 3.61 2.87 5.41
    P2O5 3.35 1.42 5.58 11.95 2.34 0.75 0.78 0.85 1.12 0.41
    LOI 5.65 5.09 4.79 5.03 6.19 6.78 2.99 3.65 2.10 5.02
    Total 99.90 99.75 99.79 99.79 99.68 99.79 99.76 99.72 99.80 99.73
    SI 0.32 13.39 6.01 16.09 15.68 5.33 12.70 7.91 10.73 19.19
    Mg# 65.30 68.77 72.94 74.01 62.79 66.83 83.66 56.23 62.65 64.61
    Sr 2214 608 1192 12.3 1024 1589 350 252 251 461
    Zr 584 112 187 263 218 348 439 344 260 231
    Ba 1565 574 2554 1287 71.5 954 982 395 469 590
    Rb 33.3 40.5 37.0 25.3 30.2 44.8 78.8 40.5 48.1 33.6
    Th 5.58 2.15 4.39 5.63 4.40 6.25 13.5 7.14 5.52 2.74
    Ta 9.12 2.28 2.89 11.0 5.05 9.04 24.2 16.7 13.5 16.3
    Nb 67.4 30.8 41.1 33.7 231 15.4 80.1 55.1 41.7 49.5
    Hf 10.9 1.65 2.75 5.11 2.87 4.94 8.35 6.90 5.25 4.29
    Y 36.0 38.9 68.7 149 62.2 49.8 25.9 24.2 21.2 19.5
    Ce 93.0 50.8 82.8 67.9 92.4 152 96.7 70.1 55.7 44.6
    Sm 7.01 5.37 8.07 10.4 9.82 13.2 8.11 7.30 5.61 6.39
    Yb 2.10 2.53 3.32 8.64 3.57 3.59 2.27 2.18 1.75 1.47
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  • [1]

    任向文.西太平洋富钴结壳成矿系统[D].青岛:中国科学院海洋研究所,2005:64-67.

    [2]

    Epp D.Possible perturbations to hotspot traces and implications for the origin and structure of the Line Islands[J].Journal of Geophysical Research,1984,89:11273-11286. doi: 10.1029/JB089iB13p11273

    [3]

    Lonsdale P.Geography and history of the Louisville hotspot chain in the Southwest Pacific[J].Journal of Geophysical Research,1988,93(B4):3078-3104.doi:10.1029/JB093iB04p03078

    [4]

    Wessel P,Kroenke L.A geometric technique for relocating hotspots and refining absolute plate motions[J].Nature,1997,387(6631):365-369. doi: 10.1038/387365a0

    [5]

    Koppers A A P,Staudigel H,Pringle M S,et al.Short-lived and discontinuous intraplate volcanism in the South Pacific:Hot spots or extensional volcanism?[J].Geochemistry Geophysics Geosystems,2003,4(10):1-49. http://www.onacademic.com/detail/journal_1000035770169610_539f.html

    [6]

    Koppers A A P,Staudigel H,Wijbrans J R,et al.The Magellan seamount trail:implications for Cretaceous hotspot volcanism and absolute Pacific plate motion[J].Earth and Planetary Science Letters,1998,163(1-4):53-68. doi: 10.1016/S0012-821X(98)00175-7

    [7]

    何高文,赵祖斌,朱克超,等.西太平洋富钴结壳资源[M].北京:地质出版社,2001.

    [8]

    Staudigel H,Park K H,Pringle M,et al.The longevity of the South Pacific Isotope and Thermal Anomaly[J].Earth and Planetary Science Letters,1991,102(1):24-44.doi:10.1016/0012-821X(91)90015-A

    [9]

    Koppers A A P,Staudigel H,Christie D M,et al.Sr-Nd-Pb Isotope Geochemistry of Leg 144 West Pacific guyots:implications for the geochemical evolution of the ‘SOPITA’ mantle anomaly[C]// Haggerty J A,Premoli Silva I,Rack F,et al.Proc.ODP Leg 144,1995:535-545.

    [10]

    Koppers A A P.40Ar/39Ar geochronology and isotope geochemistry of the West Pacific seamount province:implications for Pacific plate motion and chemical geodynamics[D].Amsterdam:Vrije Universiteit Amsterdam,1998:263.

    [11]

    陈建林,马维林,武光海,等.中太平洋海山富钴结壳与基岩关系的研究[J].海洋学报,2004,26(4):71-79. doi: 10.3321/j.issn:0253-4193.2004.04.008

    [12]

    Basaltic Volcanism Study Project.Basaltic volcanism on the terrestial planets[M].New York:Progamon Press,1981:1286.

    [13]

    Wilson M.Igneous Petrogenesis[M].London:Unwin Hyman,1989:21-22.

    [14]

    王春生,马维林,李振韶,等.DY115-17B航次报告[R].2008.

    [15]

    初凤友,李振韶,武光海,等.DY115-18航次报告[R].2008.

    [16]

    马维林,李振韶,倪建宇,等.DY115-19航次报告[R].2009.

    [17]

    Winchester J A,Floyd P A.Geochemical discrimination of different magma series and their differentiation products using immobile elements[J].Chemical Geology,1977,20(C):325-343. http://www.sciencedirect.com/science/article/pii/0009254177900572

    [18]

    Pearce J A.Role of the sub-continental lithosphere in magma genesis at active continental margins[M]//Hawkesworth C J,Norry M J.Continental Basalts and Mantle Xenoliths.Nantwish:Shiva,1983:230-249.

    [19]

    Sun S S,McDonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[C]// Saunders A D,Norry M J.Magmatism in Ocean Basins.Londn:Geol.Soc.Spec.Publ.,1989:313-345.

    [20]

    Wood D A.The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province[J].Earth and Planetary Science Letters,1980, 50:11-30. doi: 10.1016/0012-821X(80)90116-8

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收稿日期:  2017-03-27
刊出日期:  2017-12-28

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