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Estimation of S-wave velocity structure of deep soils using waveform inversion for S-wave part of earthquake ground motion from small event

机译:小事件地震地震动S波部分波形反演估算深层土壤S波速度结构

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We propose an inversion method for estimation of a 1D S-wave velocity structure of deep sedimentary layers using S-wave parts of earthquake records for evaluating site amplification. Genetic algorithm is used in inversion to find an optional model that has the minimum misfit between observed and calculated S-waves. We conducted numerical experiments using synthetic data. We applied our method to actual data at Narita in the Kanto basin and at stations around Lake Biwa. Effectiveness of the proposed methods were confirmed in the numerical experiments and actual applications
机译:我们提出了一种反演方法,该方法利用地震记录的S波部分估算深部沉积层的一维S波速度结构,以评估场地放大率。反演中使用遗传算法来找到一个可选模型,该模型在观察到的和计算出的S波之间具有最小的失配。我们使用合成数据进行了数值实验。我们将我们的方法应用于关东盆地成田和琵琶湖周围站点的实际数据。数值实验和实际应用证实了所提方法的有效性。

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