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利用钻孔体应变同震应变波测定大震震级
The seismic magnitude determination using the observation data of co-seismic strain waves from drill-hole volume strain meter
【摘要】 利用钻孔体应变仪记录的全球大震,导出同震应变波参考震级m、双振幅A、应变波推移时间τ(在短周期地震仪上测量的P波起算)的关系式m=3.0+1.40lgτ+lgA,并取得以M震级为基准的尾波应变震级标度MD=4.08+1.04lgτ+0.74lgA,尾波的多点测量改善了7.0级以上大震MD的精度,与M比较的震级标准差为0.12,MD的震级标准差为0.10,该方法测量全球大震不存在震级"饱和"问题。
【Abstract】 We use the data of drill-hole volume strain meter to determine the magnitudes of strong earthquakes around the world. We derive formulae as following: m = 3. 0 + 1. 4logτ + log A and Md= 4. 08 + 1. 04lgτ + 0. 74 lgA.In these formulae,the seismic parameters include seismic magnitude m,double amplitude A and delay time τ. The multi-points pickings up from the coda waves improve significantly the MDmagnitude precision of strong earthquake over 7. 0. The standard deviation of MDis 0. 10 seismic scale units. When we use this method to calculate the seismic magnitude of strong earthquakes,there is no saturation problem of seismic magnitude.
【Key words】 a volume strain; co-seismic strain wave; strong earthquake; seismic magnitude;
- 【文献出处】 四川地震 ,Earthquake Research in Sichuan , 编辑部邮箱 ,2015年02期
- 【分类号】P315.6
- 【被引频次】1
- 【下载频次】17