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2D Synthetic dataset of numerical simulations of long-period seismicity in a volcanic edifice and related sensitivity kernels

机译:火山大厦长期地震性数值模拟的2D合成数据集及相关灵敏核

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摘要

This work describes the data used in the EPSL research article “Quantifying strong seismic propagation effects in the upper volcanic edifice using sensitivity kernels”. The dataset is generated in order to investigate to what extent the seismic signals recorded on volcanoes are affected by near surface velocity structure. Data were calculated using the computational spectral elements scheme SPECFEM2D, where the wave propagation beneath Mount Etna volcano, Italy, was simulated in both homogeneous and heterogeneous models. The heterogeneous model comprises a low-velocity superficial structure (top several hundred meters) based on the previously published studies. Several different source mechanisms and locations were used in the simulations. The seismic wavefield was “recorded” by 15 surface receivers distributed along the surface of the volcano. The associated sensitivity kernels were also computed. These kernels highlight the region of the velocity model that affects the recorded seismogram within a desired time window. The text files describing the velocity models used in the simulations are also provided. The data may be of interest to volcano seismologists, as well as earthquake seismologists studying path effects and wave propagation through complex media.
机译:这项工作描述了EPSL研究制品中使用的数据“使用灵敏度核来量化上火山大厦的强烈地震传播效应”。生成数据集以调查在火山上记录的地震信号的程度受到近表面速度结构的影响。使用计算光谱元素方案SpecFem2D计算数据,其中在均匀和异构模型中模拟了意大利埃特纳火山下方的波传播。异构模型包括基于先前公布的研究的低速浅表结构(几百米)。在模拟中使用了几种不同的源机制和位置。通过沿着火山的表面分布的15个表面接收器“记录”地震波场。还计算了相关的灵敏度内核。这些核突出显示影响所需时间窗口中记录的地震图的速度模型的区域。还提供了描述模拟中使用的速度模型的文本文件。 Volcano地震师的数据可能感兴趣,以及通过复杂媒体研究路径效果和波传播的地震地震师。

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