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    南极洲普里兹湾岩石圈各向异性:海底地震仪观测

    牛雄伟 高金耀 吴招才 阮爱国 卫小冬 刘晨光 李天光 沈中延 潘少军 罗孝文

    牛雄伟, 高金耀, 吴招才, 阮爱国, 卫小冬, 刘晨光, 李天光, 沈中延, 潘少军, 罗孝文, 2016. 南极洲普里兹湾岩石圈各向异性:海底地震仪观测. 地球科学, 41(11): 1950-1958. doi: 10.3799/dqkx.2016.135
    引用本文: 牛雄伟, 高金耀, 吴招才, 阮爱国, 卫小冬, 刘晨光, 李天光, 沈中延, 潘少军, 罗孝文, 2016. 南极洲普里兹湾岩石圈各向异性:海底地震仪观测. 地球科学, 41(11): 1950-1958. doi: 10.3799/dqkx.2016.135
    Niu Xiongwei, Gao Jinyao, Wu Zhaocai, Ruan Aiguo, Wei Xiaodong, Liu Chenguang, Li Tianguang, Shen Zhongyan, Pan Shaojun, Luo Xiaowen, 2016. Lithosphere Anisotropy of Prydz Bay, Antarctica: From Ocean Bottom Seismometer Long Term Observation. Earth Science, 41(11): 1950-1958. doi: 10.3799/dqkx.2016.135
    Citation: Niu Xiongwei, Gao Jinyao, Wu Zhaocai, Ruan Aiguo, Wei Xiaodong, Liu Chenguang, Li Tianguang, Shen Zhongyan, Pan Shaojun, Luo Xiaowen, 2016. Lithosphere Anisotropy of Prydz Bay, Antarctica: From Ocean Bottom Seismometer Long Term Observation. Earth Science, 41(11): 1950-1958. doi: 10.3799/dqkx.2016.135

    南极洲普里兹湾岩石圈各向异性:海底地震仪观测

    doi: 10.3799/dqkx.2016.135
    基金项目: 

    极地海洋环境监测网系统研发及示范项目 201305035

    南极周边海洋地球物理考察项目 CHARE2015-01-03

    南极环境综合分析与评价项目 CHARE2015-04-01

    西南印度洋洋中脊热液成矿过程与硫化物矿区预测下属课题 2012CB417301

    国家海洋局第二海洋研究所基本科研业务费专项资金 SZ1518

    国际海域资源调查与开发“十二五”前沿性课题 DY125-22-QY-03

    国家海洋局极地考察办公室对外合作支持项目 201610

    国家自然科学基金重大研究计划重点支持项目 91228205

    详细信息
      作者简介:

      牛雄伟(1986-),助理研究员,研究方向为洋中脊和大陆边缘海底地震仪探测.E-mail: xwniu@sio.org.cn

      通讯作者:

      高金耀, E-mail: jygao@mail.hz.zj.cn

    • 中图分类号: P315.2

    Lithosphere Anisotropy of Prydz Bay, Antarctica: From Ocean Bottom Seismometer Long Term Observation

    • 摘要: 为了研究南极普里兹湾岩石圈深部应力场及其动力学,采用S波分裂旋转相关法,对中国第31次南极科学考察成功回收的3个站位海底地震仪数据(5个远震记录)进行了反演,获得了普里兹湾洋陆过渡带岩石圈各向异性特征.结果表明,台站所在区域各向异性显著,在较小的范围内存在明显的空间差异,快S波偏振方向变化范围是N40°E ~ N60°E,快慢波时间延迟变化范围为0.2~1.3 s.洋盆的各向异性主要取决于海底扩张地幔流作用,大陆及附近的各向异性主要受上地幔顶部残留构造的影响,而中间过渡带各向异性层厚度较小集中在地壳内,它可能受海底扩张地幔流和残留构造共同作用.

       

    • 图  1  (a)研究区在全球的位置和地震震中分布,(b)OBS站位分布

      SEIR的扩张方向为NE-SW向(Baran et al., 2005)

      Fig.  1.  (a) The location of study area and the positions of earthquake hypocenters, (b) positions of OBSs for long term earthquake observation

      图  2  OBS2站位事件2的波形

      Fig.  2.  The waveform of earthquake No. 2 recorded by OBS2

      图  3  OBS1站位事件2的S波分裂反演结果及分析

      a.旋转相关计算前的快慢波波形;b.旋转相关计算后的快慢波波形;c.旋转相关计算前的质点运动轨迹;d.旋转相关计算后的质点运动轨迹;e.反演结果,横轴δt为时间延迟,纵轴φ为偏振方向,两个极值点分别代表快波(δt>0) 和慢波(δt<0) 的结果,极值点对应的纵轴值分别为快波和慢波的偏振方向,横轴值分别为快慢波的时间延迟.如e图中快慢波的时间延迟为0.9 s,快波方向为N42°E,慢波方向为N138°E

      Fig.  3.  S wave splitting inversion results and analysis for earthquake No. 2 recorded by OBS1

      图  4  OBS1站位事件3的S波分裂反演结果及分析

      相关说明同图 3;e图中的快慢波时间延迟为0.8 s,快S波偏振方向为N40°E

      Fig.  4.  S wave splitting inversion results and analysis for earthquake No. 3 recorded by OBS1

      图  5  OBS2站位事件2的S波分裂反演结果及分析

      相关说明同图 3;e图中的快慢波时间延迟为0.4 s,快S波偏振方向为N44°E

      Fig.  5.  S wave splitting inversion results and analysis for earthquake No. 2 recorded by OBS2

      图  6  OBS5站位事件2的S波分裂反演结果及分析

      相关说明同图 3;e图中的快慢波时间延迟为0.2 s,快S波偏振方向为N56°E

      Fig.  6.  S wave splitting inversion results and analysis for earthquake No. 2 recorded by OBS5

      图  7  普里兹湾区域S波分裂反演得到的快波方向和时间延迟

      陆地台站的信息来源于Reading and Heintz(2008)

      Fig.  7.  S wave splitting inversion results of fast wave polarization directions and the times delay between fast and slow waves at Prydz bay

      表  1  地震事件与S波分裂反演结果

      Table  1.   Earthquake events and S wave splitting inversion results

      地震事件编号 发震时间
      (格林威治时间)
      纬度(°) 经度(°) 震源深度(km) 地震震级(Ms) OBS1 OBS2 OBS5
      d1 φ1 t1 d2 φ2 t2 d5 φ5 t5
      1 2013-04-06
      T04:42:35.860Z
      -3.517 138.476 66.0 7.0 77.314 - - 77.200 44 0.2 77.795 52 0.5
      2 2013-05-23
      T17:19:04.750Z
      -23.009 -177.232 173.7 7.4 76.884 42 0.9 76.683 44 0.4 76.046 56 0.2
      3 2013-06-05
      T04:47:26.240Z
      -11.401 166.299 39.0 6.1 81.023 40 0.8 80.989 - - 80.840 - -
      4 2013-06-16
      T02:51:35.750Z
      -56.280 -27.443 91.2 5.5 44.287 40 1.3 43.947 - - 42.998 - -
      5 2013-07-15
      T14:03:39.880Z
      -60.857 -25.070 11.0 7.3 39.879 - - 39.521 - - 38.522 60 0.8
        注:d1,d2,d5分别代表OBS1,OBS2和OBS5对某一地震事件的震中距,单位为°;φ1,φ2,φ5分别代表OBS1,OBS2和OBS5对某一地震事件的快波方位角,单位为°;t1,t2,t5分别代表OBS1,OBS2和OBS5对某一地震事件的快慢波时间延迟,单位为s;“-”为未记录或未得到结果.
      下载: 导出CSV
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