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观测到的小与大M_L/M_W标度突然改变的理论基础
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  • 英文篇名:Theoretical basis for the observed break in M_L/M_W scaling between small and large earthquakes
  • 作者:N.Deichmann ; 杨国栋 ; 曾文浩
  • 英文作者:N.Deichmann;
  • 中文刊名:世界地译丛
  • 英文刊名:Translated World Seismology
  • 机构:甘肃省地局;
  • 出版日期:2018-11-20
  • 出版单位:世界地译丛
  • 年:2019
  • 期:01
  • 基金:甘肃省地局科技发展基金项目(2016Y03)资助
  • 语种:中文;
  • 页:3-22
  • 页数:20
  • CN:11-2368/P
  • ISSN:1003-3238
  • 分类号:P315.7
摘要
对完全弹性介质中的一组地,如果应力降和破裂速度不随级系统变化,进行仪器响应校正后,在可以确定M_L的整个范围内,M_L∝M_W。然而,实际上我们观察到,M_L和M_W偏离了1:1的标度关系。天然地序列和诱发地活动实例的详细分析结果表明:对小地(通常M_W小于2~3),M_L∝1.5 M_W,这和其他研究结果一致。由独立测定若干Q值确定的因果算子Q和合成地震震源时函数褶积可以再生这一比例关系。数据分析和模拟试验的一个重要结果是,观察到的低于某一确定级的小地的脉冲宽度及其相应的拐角频率实际上是不变的。因此,在衰减介质中,小地信号本质上构成了由地矩来量度其尺度的介质的脉冲响应。简单的理论分析结果表明,在这种情况下,观察到的M_L和M_W之的比例系数1.5是矩率函数振幅和持续时对地矩固有标度特征和衰减介质频率响应的自然结果。因为这个结果和伍德—安德森地仪响应对大地引入的偏差,基于M_L的古登堡—里克特关系失去了物理上的合理性,相对于M_W导致了大地和小地不同的b值。
        
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