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Seismic Discrimination of the May 11, 1998 Indian Nuclear Test with Short-period Regional Data from Station NIL (Nilore, Pakistan)

机译:1998年5月11日印度核试验的地震判别,其中包括NIL站的短期区域数据(巴基斯坦尼洛尔)

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Regional seismic discriminants for the May 11, 1998 Indian underground nuclear test(s) and earthquakes recorded at station NIL (Nilore, Pakistan) provide new data to test strategies that can be used to monitor the Comprehensive Nuclear-Test-Ban Treaty (CTBT). Three categories of regional discriminants (ratios of P- and/or S-wave energy) were measured on short-period (0.5-6 Hz) seismograms: P/S amplitude ratios (phase ratios) measured in the same frequency band, P- and S-wave spectral ratios (i.e., low frequency to high frequency for the same phase) and P/S cross-spectral ratios (i.e., low frequency S-wave to high frequency P-wave). The P/S amplitude ratios show good separation of the Indian nuclear test and regional earthquakes for Pn/Lg and Pn/Sn, however Pg/Lg does not discriminate as well. Pn/Lg and Pn/Sn discriminate well at frequencies as low as 0.5-2 Hz, especially after accounting for path effects. This observation differs from previous studies that report poor separation of earthquakes and explosions at lower frequencies. The P/S amplitude ratios do not show any magnitude dependence, suggesting that forming the ratios in a fixed frequency band cancels the effects of source size-corner frequency scaling. Spatial variability of the observed discriminants arises from variations in crustal waveguide and/or attenuation structure (path propagation effects). Grouping amplitude ratios for earthquakes with paths similar to the Indian test greatly improves discrimination. Removing distance trends does not generally improve discrimination. Accounting for path effects with Bayesian kriging significantly improves discrimination. Spectral ratios (e.g., Pn [0.5-1 Hz]/Pn [4-6 Hz]) and cross-spectral ratios (e.g., Lg [1-2 Hz]/Pn [4-6 Hz]) show distance and magnitude dependence. We developed a technique for simultaneously removing the effects of distance and source size-corner frequency scaling on amplitude and spectral ratios. The technique uses a gridsearch to find several parameters that characterize the observed distance and magnitude dependence. Discrimination of the Indian test improved dramatically after the distance and magnitude trends were removed from the spectral and cross-spectral ratio data.
机译:1998年5月11日印度地下核试验的区域地震判别和在NIL站(巴基斯坦尼洛尔)记录的地震为试验策略提供了新数据,可用于监测《全面禁止核试验条约》(CTBT) 。在短周期(0.5-6 Hz)地震图中测量了三类区域判别式(P波和/或S波能量的比):在相同频段测量的P / S振幅比(相位比),P- S和S波的频谱比(即,同一相位的低频到高频)和P / S互谱比(即,低频S波和高频P波)。 P / S振幅比显示印度核试验和区域地震对Pn / Lg和Pn / Sn的良好分隔,但是Pg / Lg也没有区别。在低至0.5-2 Hz的频率下,Pn / Lg和Pn / Sn可以很好地区分,尤其是考虑到路径效应之后。该观察结果不同于以前的研究,后者报告了较低频率下地震和爆炸的分离差。 P / S振幅比不显示任何幅度依赖性,这表明在固定频带中形成比率会抵消源尺寸角频率缩放的影响。观测到的判别式的空间变异性是由地壳波导和/或衰减结构的变异(路径传播效应)引起的。将路径类似于印度测试的地震的振幅比进行分组,可以大大提高判别力。消除距离趋势通常不会改善歧视。用贝叶斯克里金法计算路径效应可以显着改善辨别力。光谱比(例如,Pn [0.5-1 Hz] / Pn [4-6 Hz])和交叉光谱比(例如,Lg [1-2 Hz] / Pn [4-6 Hz])显示距离和幅度的依赖性。我们开发了一种技术,可同时消除距离和源大小角频率缩放对幅度和频谱比的影响。该技术使用网格搜索来找到表征观察到的距离和幅度依赖性的几个参数。从光谱和互谱比数据中删除了距离和幅度趋势后,对印度测试的区分得到了显着改善。

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