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    花东海盆综合地震探测及其重要的构造意义

    赵明辉 王强 杨富东 张佳政 高红芳 孙龙涛 刘思青 张光学

    赵明辉, 王强, 杨富东, 张佳政, 高红芳, 孙龙涛, 刘思青, 张光学, 2021. 花东海盆综合地震探测及其重要的构造意义. 地球科学, 46(1): 359-368. doi: 10.3799/dqkx.2020.038
    引用本文: 赵明辉, 王强, 杨富东, 张佳政, 高红芳, 孙龙涛, 刘思青, 张光学, 2021. 花东海盆综合地震探测及其重要的构造意义. 地球科学, 46(1): 359-368. doi: 10.3799/dqkx.2020.038
    Zhao Minghui, Wang Qiang, Yang Fudong, Zhang Jiazheng, Gao Hongfang, Sun Longtao, Liu Siqing, Zhang Guangxue, 2021. Seismic Survey in Huatung Basin and Its Tectonic Significance. Earth Science, 46(1): 359-368. doi: 10.3799/dqkx.2020.038
    Citation: Zhao Minghui, Wang Qiang, Yang Fudong, Zhang Jiazheng, Gao Hongfang, Sun Longtao, Liu Siqing, Zhang Guangxue, 2021. Seismic Survey in Huatung Basin and Its Tectonic Significance. Earth Science, 46(1): 359-368. doi: 10.3799/dqkx.2020.038

    花东海盆综合地震探测及其重要的构造意义

    doi: 10.3799/dqkx.2020.038
    基金项目: 

    国家自然科学基金项目 91958212

    国家自然科学基金项目 41730532

    国家自然科学基金项目 91428204

    国家自然科学基金项目 41376063

    广东省基金团队项目 2017A030312002

    国家自然科学基金委员会共享航次 NORC2020-581

    详细信息
      作者简介:

      赵明辉(1967-), 女, 研究员, 主要从事海洋地球物理与深部结构研究.ORCID:0000-0003-0848-9210.E-mail:mhzhao@scsio.ac.cn

    • 中图分类号: P731.1

    Seismic Survey in Huatung Basin and Its Tectonic Significance

    • 摘要: 花东海盆位于欧亚板块与菲律宾海板块交汇处,是现今西太平洋俯冲体系中唯一遗留的早白垩纪洋盆,是研究西太平洋俯冲构造演化与动力学机制的一个关键区域.前期研究发现,关于花东海盆的基础科学问题迫切需要解决:花东海盆的性质、年龄及形成演化历史如何?南北走向的加瓜海脊是花东海盆的东部边界吗?其隆升机制和构造属性如何?花东海盆的西部边界是马尼拉俯冲带吗?其各构造单元流体作用及其与花东海盆的构造关系如何?为了解决上述科学问题,在花东海盆开展主动源与被动源的综合地球物理探测和地质采样是非常必要的.一方面,可以采用纵/横波联合反演方法获取花东海盆及其东/西边界的深达地幔的精细速度结构,为构建西太平洋俯冲构造体系跨圈层的构造演化模式提供重要的地质地球物理证据,另一方面,为中国未来在花东海盆大洋钻探计划提供重要的基础数据.

       

    • 图  1  花东海盆区域构造位置与水深地形

      黄色方框为图 2范围

      Fig.  1.  The regional tectonic map and bathymetric topography of Huatung basin

      图  2  花东海盆及邻区的深地震探测现状

      OBS1995、OBS2015⁃2、T1⁃T5测线、OBS2016⁃2和三维网格3D⁃2016测线为研究区已有的OBS深地震测线;白色实线为10条长缆多道反射测线(H1⁃H8, V1⁃V2);粉红色实线是MCS973反射地震剖面.黄星(RD19和RD20)为辉长岩样品位置;绿色圆为IODP井位DSDP293

      Fig.  2.  Locations of deep seismic profiles in the Huatung basin and adjacent areas

      图  3  花东海盆TAIGER计划中4条测线初至波层析成像速度结构图

      Eakin et al.(2015).a、b、c和d分别为T5、T4A、T2和T1b测线的速度结构,测线位置见图 2;白色虚线和M是根据反射剖面推测的Moho界面;HB:花东海盆;GA:加瓜海脊;NLA:北吕宋岛弧;WPB:西菲律宾海盆

      Fig.  3.  First⁃arrival tomographic models along T1b, T2, T4A and T5 profiles across Huatung Basin in TAIGER plan

      图  4  加瓜海脊形成机制示意图

      Deschamps et al.(1998)

      Fig.  4.  The schematic diagram of the Gagua Ridge Formation

      图  5  花东海盆及其东/西部板块边界的三维海底地形图及各圈层相互作用示意图

      Tian et al.(2019)修改

      Fig.  5.  Three⁃dimensional topographic map of Huatung basin and schematic diagram of multi⁃layers interaction

      图  6  花东海盆综合深地震探测建议部署图

      basin白色粗线为人工源地震测线OBS 2020,红色圆为短周期OBS,共布放31台,OBS间距7 km;黑色圆为7台宽频带长周期OBS,放置海底6~8个月,用于记录天然地震数据;红色锯齿实线为琉球海沟板片边界;红色五角星为6个地质拖网/浅钻采样点

      Fig.  6.  The suggested deployment map of comprehensive deep seismic survey of the Huatung

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