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    海南岛东南海域碎屑锆石年代学物源示踪及构造指示意义

    刘松峰 李顺 聂鑫 邹俪琦 蔡观强

    刘松峰, 李顺, 聂鑫, 邹俪琦, 蔡观强, 2021. 海南岛东南海域碎屑锆石年代学物源示踪及构造指示意义. 地球科学, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024
    引用本文: 刘松峰, 李顺, 聂鑫, 邹俪琦, 蔡观强, 2021. 海南岛东南海域碎屑锆石年代学物源示踪及构造指示意义. 地球科学, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024
    Liu Songfeng, Li Shun, Nie Xin, Zou Liqi, Cai Guanqiang, 2021. Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications. Earth Science, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024
    Citation: Liu Songfeng, Li Shun, Nie Xin, Zou Liqi, Cai Guanqiang, 2021. Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications. Earth Science, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024

    海南岛东南海域碎屑锆石年代学物源示踪及构造指示意义

    doi: 10.3799/dqkx.2021.024
    基金项目: 

    中国地质调查局地质调查项目 DD20190627

    中国地质调查局地质调查项目 DD20190209

    中国地质调查局地质调查项目 DD20190577

    中国地质调查局地质调查项目 DD20190378

    中国地质调查局地质调查项目 DD20190366

    南方海洋与工程广东省实验室(广州)人才引进重大专项 GML2019ZD0201

    南方海洋与工程广东省实验室(广州)人才引进重大专项 GML2019ZD0207

    详细信息
      作者简介:

      刘松峰(1987-), 男, 工程师, 博士, 主要从事海洋地质调查与岩石成因大地构造研究.ORCID: 0000-0002-3220-5436.E-mail: liusongfeng_cug@163.com

      通讯作者:

      蔡观强, ORCID: 0000-0002-0236-089X.E-mail: caiguanqiang@sina.com

    • 中图分类号: P67

    Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications

    • 摘要: 为探索海南岛东南海域表层沉积物来源,揭示物源区主要地质构造演化事件,采用箱式取样法获取8个站位沉积物样品,进行锆石U-Pb定年.结果表明,773个有效年龄分布在33~3 205 Ma,主要年龄峰集中在燕山期(100 Ma、140 Ma和159 Ma)、印支期(242 Ma)和加里东期(439 Ma),次要年龄峰集中在新元古代(776 Ma、965 Ma)和古元古代(1 836 Ma、2 487 Ma),并零星保留太古宙基底年龄信息.少量变质锆石记录了加里东期和印支期强烈的变质事件.与潜在物源区对比分析表明,海南岛东南海域沉积物以约100 Ma的年龄峰值为识别标志,主要来源于海南岛.结合前人资料,本研究年龄频谱指示加里东期华夏武夷-云开造山带可延伸到海南岛,海西-印支期古特提斯洋的闭合及印支-华夏地块的碰撞导致其强烈的构造-岩浆-变质作用,燕山期受太平洋板块俯冲的影响发育多期次岩浆活动.

       

    • 图  1  海南岛位置及周围盆地分布图(a)和海南岛地质简图(b)

      b.据陈新跃等(2011)修编

      Fig.  1.  The location of Hainan Island and distribution map of surrounding basins (a) and the simplified geological map of Hainan Island (b)

      图  2  琼东南海域表层沉积物照片

      a.青灰色细砂;b.灰色砂质粘土

      Fig.  2.  Photos of the surface sediments from southeastern sea of Hainan Island

      图  3  琼东南海域单道地震剖面

      a. ab剖面;b.cd剖面,剖面位置见图 1b

      Fig.  3.  Single channel seismic section from southeastern sea of Hainan Island

      图  4  海南岛东南海域沉积物样品代表性碎屑锆石阴极发光照片

      Fig.  4.  The cathodoluminescence images of representative detrital zircons of different sediment samples from southeastern sea of Hainan Island

      图  5  碎屑锆石U-Pb年龄和Th/U比值散点图

      Fig.  5.  Plot of U-Pb ages versus Th/U ratios of detrital zircons

      图  6  样品碎屑锆石U-Pb年龄频谱直方图及饼状图

      Fig.  6.  U-Pb age spectrum diagrams and pie graphs for detrital zircons from the studied samples

      图  7  变质锆石阴极发光图和年龄加权平均值

      Fig.  7.  The cathodoluminescence images and weighted average ages of metamorphic zircons

      图  8  不同地块和河流潜在物源区碎屑锆石U-Pb谐和年龄频谱图

      数据来源请参见Wang et al.(2018, 2019)

      Fig.  8.  Detrital zircon U-Pb age probability density plots of the bedrocks and major drainages of the potential source terranes

      图  9  海南岛东南海域样品碎屑锆石U-Pb年龄累计概率图

      Fig.  9.  Cumulative probability plot for the detrital zircon U-Pb ages of samples from the southeastern sea of Hainan Island

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