利用极化滤波和阵列分析增强地震相位识别

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
On Ki Angel Ling, Simon C. Stähler, David Sollberger, Domenico Giardini
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引用次数: 0

摘要

地震阵在识别地震波场中的弱信号方面发挥着至关重要的作用,这些信号是基于地震波场的预期慢度和反方位角值来识别的。然而,当研究具有相似水平慢度和到达时间的相位时,例如接收端或源端混响和转换相位,它们的分辨能力受到限制。因此,我们研究了在叠加前对三分量地震图进行极化滤波的好处,以去除不希望的信号并提高阵列的信噪比。定制偏振滤波器使更复杂的波场分离和可靠的相位识别。然而,选择合适的极化滤波器需要在降噪和保留所需信号之间取得平衡。我们发现偏振度滤波器通常在抑制非相干噪声方面表现优异。另一方面,一些滤波器,例如,完全基于椭圆性,对体波没有显著的增强效果,甚至可能产生不利影响,特别是对地震记录中较晚到达的相位。我们使用AlpArray和周围永久站点记录的数据来证明这些发现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Enhancement of Seismic Phase Identification Using Polarization Filtering and Array Analysis
ABSTRACT Seismic arrays play a crucial role in identifying weak signals in the seismic wavefield based on their expected slowness and backazimuth values. However, their resolution power is limited when studying phases with similar horizontal slownesses and arrival times, such as receiver-side or source-side reverberations and converted phases. Therefore, we investigate the benefit of applying polarization filtering to three-component seismograms before stacking to remove undesired signals and increase the signal-to-noise ratio of the array. Customized polarization filters enable more sophisticated wavefield separation and robust phase identification on vespagrams. However, selecting the suitable polarization filter requires a balance between noise reduction and the preservation of desired signals. We find that degree-of-polarization filters generally excel in suppressing incoherent noise. On the other hand, some filters, for example, based solely on ellipticity, do not yield notable enhancements for body waves and may even produce adverse effects, specifically for phases that arrive late in the seismogram. We demonstrate these findings using data recorded by AlpArray and surrounding permanent stations.
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来源期刊
Bulletin of the Seismological Society of America
Bulletin of the Seismological Society of America 地学-地球化学与地球物理
CiteScore
5.80
自引率
13.30%
发文量
140
审稿时长
3 months
期刊介绍: The Bulletin of the Seismological Society of America, commonly referred to as BSSA, (ISSN 0037-1106) is the premier journal of advanced research in earthquake seismology and related disciplines. It first appeared in 1911 and became a bimonthly in 1963. Each issue is composed of scientific papers on the various aspects of seismology, including investigation of specific earthquakes, theoretical and observational studies of seismic waves, inverse methods for determining the structure of the Earth or the dynamics of the earthquake source, seismometry, earthquake hazard and risk estimation, seismotectonics, and earthquake engineering. Special issues focus on important earthquakes or rapidly changing topics in seismology. BSSA is published by the Seismological Society of America.
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