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ISSN?0253-3782 CN?11-2021/P

走滑断层对洋中脊热结构与流动场的影响规律及对太平洋南部边界RRF型三联点的解释

王振山 ,? 魏东平 ,? 徐佳静 ,? 王少坡

引用本文: 王振山,?魏东平,?徐佳静,?王少坡. 2019.?走滑断层对洋中脊热结构与流动场的影响规律及对太平洋南部边界RRF型三联点的解释.?地震学报[J]. doi: 10.11939/jass.20180009 shu
Citation:? Wang Zhenshan,?Wei Dongping,?Xu Jiajing,?Wang Shaopo. 2019.?Effects of the transform fault on the temperature structure and mantle flow of the mid-ocean ridge and their interpretation to RRF triple junction at the southern Pacific boundary.?Acta Seismologica Sinica. doi: 10.11939/jass.20180009 shu

走滑断层对洋中脊热结构与流动场的影响规律及对太平洋南部边界RRF型三联点的解释

    通讯作者: 魏东平, dongping@ucas.ac.cn
摘要: 选取太平洋板块南部边界的板块相对运动速度不同的两个洋脊—洋脊—转换断层(RRF)型三联点,即麦夸里(Macquarie)三联点和南太平洋三联点为研究对象,通过数值模拟的方法,研究该类型三联点走滑断层边界两侧的板块相对运动速度对三联点附近地区地幔流动场和温度结构的影响。模拟结果表明,太平洋南部边界RRF三联点走滑断层边界两侧的板块相对运动速度控制着三联点附近的温度分布与地幔流动。随着走滑断层边界两侧板块相对运动速度的增加,转换断层相对滑动速度增加,温度上升,距洋脊边界100 km范围内的地幔流体速度变大。麦夸里三联点和南太平洋三联点处3个板块的相对运动,使得三联点的转换断层边界浅部产生剪应力集中,造成震源深度集中在15—25 km;同时相对运动产生的地幔流动造成温度结构变化,该变化控制着地形变化。

English

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  • 图?1? 三联点分布图

    Figure?1.? The distribution map of triple junctions

    图?2? RRF型三联点模型示意图

    Figure?2.? The schematic diagram of the model of RRF triple junction

    图?3? 模型1的温度结构

    Figure?3.? The temperature structure of model one

    图?4? 模拟温度与计算所得30 km深处的温度对比图

    Figure?4.? The contrast diagram of simulation temperature and calculation temperature at 30 km depth

    图?5? 模型1—9温度对比图

    Figure?5.? The temperature contrast diagram of model 1—9

    图?6? 模型1垂向地幔流体速度场

    Figure?6.? The upwelling velocity of model one

    图?7? 模型1—9在45 km深处的垂向地幔流体速度对比图

    Figure?7.? The vertical velocity contrast diagram of model 1—9 at 45 km depth

    图?8? 转换断层地形对比图

    Figure?8.? The contrast map of topography for the transform faults

    图?9? 转换断层等温线剖面图

    Figure?9.? The isothermal profile of the transform fault

    参数数值单位参数数值单位
    ρ0 3 300kg/m3CP1 200J/(kg·K)
    α 3×10?51/KT00
    η0 1×1019Pa·sTm1 300
    ηmax1×1023Pa·sC010MPa
    μ 0.6R8.314 4J/(mol·K)
    k 3W/(m·K)E260kJ/mol

    表?1? 模型参数(Behn et al,2007Georgen,2008

    Table?1.? Reference parameters of the model (Behn et al,2007Georgen,2008

    下载: 导出CSV
    模型R1/(cm·yr?1R2/(cm·yr?1F/(cm·yr?1模型R1/(cm·yr?1R2/(cm·yr?1F/(cm·yr?1
    136366126
    239676159
    331298242
    4315129583
    5693
      注:R1R2F分别为代表模型中慢速扩张洋脊、快速扩张洋脊和转换断层。

    表?2? 模型板块相对运动速度

    Table?2.? The relative velocities of plates in the models

    下载: 导出CSV
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文章相关
  • 通讯作者:? 魏东平, dongping@ucas.ac.cn
  • 收稿日期:? 2018-03-08
  • 录用日期:? 2019-03-22
  • 网络出版日期:? 2019-07-01
通讯作者: 陈斌, bchen63@163.com
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