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    洋岛-海山研究进展及其对于重建洋板块的意义

    袁四化 潘桂棠 任飞

    袁四化, 潘桂棠, 任飞, 2020. 洋岛-海山研究进展及其对于重建洋板块的意义. 地球科学, 45(8): 2826-2845. doi: 10.3799/dqkx.2020.124
    引用本文: 袁四化, 潘桂棠, 任飞, 2020. 洋岛-海山研究进展及其对于重建洋板块的意义. 地球科学, 45(8): 2826-2845. doi: 10.3799/dqkx.2020.124
    Yuan Sihua, Pan Guitang, Ren Fei, 2020. Review on Geological Research of Oceanic Island-Seamount and Its Significance for Reconstruction of Ocean Plate. Earth Science, 45(8): 2826-2845. doi: 10.3799/dqkx.2020.124
    Citation: Yuan Sihua, Pan Guitang, Ren Fei, 2020. Review on Geological Research of Oceanic Island-Seamount and Its Significance for Reconstruction of Ocean Plate. Earth Science, 45(8): 2826-2845. doi: 10.3799/dqkx.2020.124

    洋岛-海山研究进展及其对于重建洋板块的意义

    doi: 10.3799/dqkx.2020.124
    基金项目: 

    中央高校基本科研业务费 ZY20110202

    国家自然科学基金项目 41772200

    国家自然科学基金项目 91755212

    防灾科技学院精品课程建设项目 JPJS2018001

    防灾科技学院精品课程建设项目 JPJS2018005

    中国地质调查局项目 DD20190375

    中国地质调查局项目 DD20190053

    中国地质调查局项目 DD20179386

    中国地质调查局项目 DD2016G0345

    详细信息
      作者简介:

      袁四化(1980-), 男, 博士, 副教授, 主要从事区域地质研究.ORCID:0000-0002-8737-2856.E-mail:yuansihua@126.com

    • 中图分类号: P54

    Review on Geological Research of Oceanic Island-Seamount and Its Significance for Reconstruction of Ocean Plate

    • 摘要: 在中国区域大地构造研究中,对洋岛-海山/洋底高原的识别尚未引起足够重视.为深入研究中国大陆洋板块构造,系统回顾了洋岛-海山/洋底高原的基本概念、基本特征和增生造山过程.洋岛-海山/洋底高原是在海底扩张、大洋壳演化过程中由于地幔热点/柱作用形成的有异常厚度洋壳的区域,是大洋岩石圈的重要组成部分.洋岛-海山/洋底高原在垂向上具有典型的二元结构,下部以镁铁质、超镁铁质岩石为主,上部以碳酸盐岩建造为主.现今大洋盆地中大面积分布着正在演化中和正在俯冲的洋岛-海山,根据比较大地构造学原理,古洋岛-海山的存在指示古大洋盆地的存在,是研究造山带的重要载体.认为地史时期大洋盆地中有相当数量的洋岛、海山,在俯冲增生碰撞造山过程中保留下来的古洋岛-海山残块以构造岩片(块)形式夹持在俯冲增生杂岩中,随大洋盆地关闭;其作为缝合带的重要组成部分,是识别对接带的重要判别依据之一.

       

    • 图  1  全球数字地形图,显示主要洋岛-海山/洋底高原

      Amante and Eakins (2009)

      Fig.  1.  ETOPO1 ice surface global relief model, showing main oceanic island‐seamounts/oceanic plateaus

      图  2  海山地层结构模式

      Sano and Kanmera (1988)Safonova et al.(2016)

      Fig.  2.  A seamount statigraphic model reconstructed from the Akiyoshi accretionary complex

      图  3  海山的6个演化阶段

      a.小型海山;b.中型海山;c.浅海山;d.洋岛;e.平顶山;f.海山破坏.据Staudigel and Clague (2010)

      Fig.  3.  Six stages of seamount evolution

      图  4  洋底高原结构示意图

      Kerr et al.(1998)Condie (2001)

      Fig.  4.  The internal structure of oceanic plateau

      图  5  洋底高原岩石组合关系示意图

      Kerr et al.(1998)Condie (2001)

      Fig.  5.  Schematic rock column showing the inferred relationship of the different igneous rocks

      图  6  翁通-爪哇高原深海钻探及其邻区代表岩性柱

      Tarduno et al. (1991)

      Fig.  6.  Representative lithologic column of Ontong-Java plateau deep sea drilling and its adjacent area

      图  7  哥斯达黎加中部俯冲海山遥感影像显示俯冲海山的破坏形态

      a.俯冲海山刚进入增生楔;b.已进入增生楔的海山;c.几乎被增生楔覆盖的海山.底图据Google Earth,地质信息据von Huene et al.(2004)

      Fig.  7.  Remote sensing image of central Costa Rica showing disruptive morphology from subducting seamounts

      图  8  海山俯冲示意图

      Watts (2010)

      Fig.  8.  Schematic diagram illustrating the model for seamount subduction

      图  9  洋底高原与岛弧(a)和活动大陆边缘(b)碰撞示意图

      Kerr and Mahoney (2007)

      Fig.  9.  Schematic cross sections showing the possible effects of oceanic plateau collision with an island arc (a) and a subduction zone at a continental margin (b)

      图  10  马鬃山杂岩中洋岛-海山组合

      Wang et al. (2020)

      Fig.  10.  Oceanic island/seamount relics in the Mazongshan complex

      表  1  不同构造背景下火山岩层序的地球化学和地质判别特征

      Table  1.   Diagnostic geochemical and geological characteristics of volcanic sequences from different tectonic settings

      构造环境 高MgO熔岩(> 14%) 低MgO熔岩(< 3%) Nb/La 球粒陨石标准化REE配分模式 枕状熔岩 火山喷发层 陆地喷发 深海沉积夹层
      洋底高原 常见 很少 ≥1 主要平坦型 很少 偶然
      洋中脊 很少 很少 ≥1 LREE亏损型 很少 很少
      边缘海盆地 很少 很少 ≥1 主要平坦型
      洋岛玄武岩 很少 很少 ≥1 LREE富集 很少 通常 很少
      被动边缘 常见 很少 平坦型到LREE富集 并不都是熔岩枕状 偶然 通常
      很少 常见 远小于1 LREE富集 并不都是熔岩枕状 通常 很少
      大陆溢流玄武岩 常见 常见 通常远小于1,少部分≥1 平坦型到LREE富集 偶然
      注:据Kerr (2014).
      下载: 导出CSV
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