Regional Features of Seismic Wave Attenuation in the North Caucasus

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
A. S. Zvereva, I. P. Gabsatarova, D. V. Likhodeev
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引用次数: 0

Abstract—New generalized data on the attenuation of seismic waves in the lithosphere of the North Caucasus were obtained using the frequency-dependent quality factor of the medium Qs(f). Knowledge of the heterogeneities of the quality factor distribution as a characteristic of the environment in the region is necessary when carrying out seismic zoning work of varying degrees of detail. The information base for the study comprised digital records of 53 seismic stations of 800 local earthquakes with moderate magnitudes (1.8 ≤ M ≤ 5.5), evenly distributed throughout the North Caucasus. The study used the coda-wave envelope method in the single scattering model (CodaQ). For the territory of the North Caucasus and for seven individual zones, average analytical expressions of the frequency-dependent quality factor of the medium Qs(f) were calculated and maps of the distribution of quality values at frequencies of 1 and 4 Hz were compiled. It was revealed that the zones with the lowest quality factor correspond to tectonically heterogeneous regions characterized by the presence of strong fragmentation in the crust and an increased level of fluid saturation. The zones of the highest quality factor correspond to zones of lithospheric extension, where earthquakes with normal-fault focal mechanisms predominate.

Abstract Image

北高加索地区地震波衰减的区域特征
摘要利用介质Qs(f)的频率相关质量因子,获得了北高加索岩石圈地震波衰减的新的广义数据。在进行不同程度详细的地震区划工作时,了解作为该地区环境特征的质量因子分布的异质性是必要的。该研究的信息库包括53个地震台站的800次中等震级(1.8≤M≤5.5)的数字记录,这些地震均匀分布在北高加索地区。本研究采用单散射模型(CodaQ)的尾波包络法。对于北高加索领土和七个单独的区域,计算了介质q (f)的频率相关质量因子的平均解析表达式,并编制了1和4赫兹频率上质量值的分布图。结果表明,质量因子最低的区域对应于地壳破碎性强、流体饱和度高的构造非均质区。质量因子最高的区域对应于岩石圈伸展带,以正断层震源机制为主。
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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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