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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Attenuation of Lg waves in the New Madrid seismic zone of the central United States using the coda normalization method
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Attenuation of Lg waves in the New Madrid seismic zone of the central United States using the coda normalization method

机译:衰减 lg 在美国中部地区新的马德里地震区使用CODA规范化方法

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摘要

Abstract Unique properties of coda waves are employed to evaluate the frequency dependent quality factor of Lg waves using the coda normalization method in the New Madrid seismic zone of the central United States. Instrument and site responses are eliminated and source functions are isolated to construct the inversion problem. For this purpose, we used 121 seismograms from 37 events with moment magnitudes, M, ranging from 2.5 to 5.2 and hypocentral distances from 120 to 440km recorded by 11 broadband stations. A singular value decomposition (SVD) algorithm is used to extract Q values from the data, while the geometric spreading exponent is assumed to be a constant. Inversion results are then fitted with a power law equation from 3 to 12Hz to derive the frequency dependent quality factor function. The final results of the analysis are Q V Lg (f)=(410±38) f 0.49±0.05 for the vertical component and Q H
机译:<![cdata [ 抽象 用于评估 Lg 使用CODA归一化方法在美国中部新的马德里地震区。储存仪器和站点响应,孤立源功能以构建反转问题。为此目的,我们使用了来自37个事件的121个地震图,其中瞬间大小, m ,从2.5到5.2和440的斜视距离 km录制11个宽带站。 奇异值分解(SVD)算法用于提取 q 来自数据的值,而假设几何扩展指数是常数。然后,反转结果将电源法方程从3到12 Hz配合,以导出频率依赖性质量因子函数。分析的最终结果是 q v lg f = (410 ± 38) f 0.49 ± 0.05 用于垂直组件和 q h

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