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芦山地震断层滑动速度的计算
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  • 英文篇名:Fault sliding velocity computation of Lushan earthquake
  • 作者:李启成 ; 郭雷 ; 何书耕 ; 姜胜友 ; 宋杰城 ; 庄园 ; 张成城 ; 崔亮亮
  • 英文作者:LI Qi-cheng;GUO Lei;HE Shu-geng;JIANG Sheng-you;SONG Jie-cheng;ZHUANG Yuan;ZHANG Cheng-cheng;CUI Liang-liang;Department of Geology Liaoning Technical University;
  • 关键词:多普勒效应 ; 滑动速度函数 ; 断层 ; 地震 ; 芦山
  • 英文关键词:Doppler effect;;sliding velocity function;;fault;;earthquake;;Lushan
  • 中文刊名:DQWJ
  • 英文刊名:Progress in Geophysics
  • 机构:辽宁工程技术大学;
  • 出版日期:2017-12-29 17:49
  • 出版单位:地球物理学进展
  • 年:2018
  • 期:v.33;No.147
  • 基金:辽宁省教育厅项目“LJYL040断层滑动速度研究”(551610001219)资助
  • 语种:中文;
  • 页:DQWJ201801008
  • 页数:6
  • CN:01
  • ISSN:11-2982/P
  • 分类号:57-62
摘要
以往得到的断层滑动速度函数要么是通过理论研究获得的,要么是计算的结果与地壳介质等因素有关.由于目前人们对地壳介质和震源机制研究的局限性,使得计算结果的准确性不高.在系统提出用多普勒效应计算断层滑动速度函数的基础上,以芦山地震余震为例计算了地震断层的滑动速度函数.结果表明:滑动速度函数具有迅速上升,相对缓慢下降的特点,与我们以往的计算结果一致,也与Hisada的研究结果一致.用多普勒效应计算断层断层滑动速度函数的结果与地壳介质和震源机制无关,应该是一种有前途的计算地震断层滑动速度的方法.
        The fault sliding velocity function was acquired either from theory or from computational results that have something to do with crust medium and other factor. Limitations that people understand the crust medium and source mechanism make accuracy of computational results low. On the basis of our systemic method that computes fault sliding velocity function with Doppler effect,fault sliding velocity function of Lushan aftershock is calculated.Computational results show fault sliding velocity function has characteristic that velocity raises rapidly,and descends slowly,these results are identical with our computation before,and identical with Hisada. The computational results by Doppler effect have nothing to do with the crust medium and source mechanism,so this method is effective to calculate fault sliding velocity function.
引文
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