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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