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首页> 外文期刊>Journal of seismology >An approach of refraction seismology for processing and modeling of local earthquake seismogram sections of virtual sources at multiple depths in seismogenic regions-application to Koyna-Warna region, India, for upper crustal P and S velocity structure
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An approach of refraction seismology for processing and modeling of local earthquake seismogram sections of virtual sources at multiple depths in seismogenic regions-application to Koyna-Warna region, India, for upper crustal P and S velocity structure

机译:一种折射热理学方法,用于处理和建模局部地震地震源在地震区施用中的虚拟源局部应用对印度Koyna-Warna地区的应用,用于上层地壳P和S速度结构

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摘要

We present an approach based on controlled source seismology (CSS) methods, especially developed for processing and modeling of the local earthquake seismograms. Record sections of the local earthquake seismograms generated for multiple source depths illuminate the upper crustal velocity structure in the region. Extensive travel times and synthetic seismograms modeling of the observed record sections reveal the P and S velocity structure in the region. The strength of this approach essentially lies with the possibility of validating the upper crustal velocity models inferred in various subregions of the seismogenic region. A redundant and significantly large number of virtual source local earthquake seismogram sections, gathered for multiple source depths and varying source mechanisms in each of the subregions, validate the same set of P and S velocity models in that region. Further, those models are found to generate the synthetic seismograms consistent with the observed sections. The proposed approach effectively utilizes a reliable dataset from a great volume of well-located local earthquake recordings of a state-of-the-art digital seismograph network. Such a dataset of local earthquake seismograms in the Koyna-Warna active earthquake zone is used here to demonstrate this approach and obtained subregion-specific models of upper crustal P and S velocity structure in the epicentral region. The results indicate that the technique presented here is efficient for processing and modeling the local earthquake seismograms and deriving upper crustal velocity models in the seismogenic regions.
机译:我们提出了一种基于受控源地震学(CSS)方法的方法,特别是为当地地震地震图的加工和建模而开发。为多个源深度产生的局部地震地震图的记录部分照亮了该区域的上层地壳速度结构。观察到的记录部分的广泛旅行时间和合成地震图建模揭示了该地区的P和S速度结构。该方法的强度基本上呈现验证在发源地区的各种亚区中推断的上层地壳速度模型的可能性。冗余和显着大的虚拟源局部地震地震图部分,聚集在每个子区域中的多个源深度和不同的源机制,验证该区域中的相同组P和S速度模型。此外,发现这些模型产生与观察到的部分一致的合成地震图。所提出的方法有效地利用了来自最先进的数字地震网络的大量众多局部地震记录的可靠数据集。这里使用了Koyna-Warna主动地震区中的当地地震地震图的这种数据图来证明这种方法,并在显着区域中获得了上层地壳P和S速度结构的子区域特异性模型。结果表明,这里呈现的技术是在局部地震地震图中加工和建模局部地震地震表谱和衍生出泻种子地区的地壳速度模型的有效技术。

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