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S-wave velocity structure of Mexico City obtained from three- component microtremor measurements and microtremor array measurements

机译:从三组分MicroTremor测量获得的墨西哥城的S波速度结构和微反线阵列测量

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Three-component microtremor measurements and microtremor array measurements have been performed at 6 points in central Mexico City. The microtremor array measurements used 25 to 650 m triangular arrays and clear dispersion curves were obtained between 0.3 and 10 Hz. The peak frequencies of the Horizontal and Vertical ratio (H/V) of spectra vary from 0.25 to 2 Hz. A joint inversion of an H/V spectrum and a dispersion curve is applied to observed data and S-wave velocity models down to a depth of 200 m were obtained. A low velocity layer with S-wave velocity lower than 150 m/s existed at a depth of 70 m at the middle of the Mexico basin. It seems that the peak frequency of 0.25 Hz in the H/V spectra is due to this shallow low velocity layer.
机译:在墨西哥城中部的6个点上进行了三个组分的微反线测量和MicroTremor阵列测量。在0.3和10Hz之间获得25至650 m三角形阵列和清晰的分散曲线使用的微反射阵列测量。光谱的水平和垂直比(H / V)的峰值频率从0.25到2 Hz变化。将H / V光谱的关节反转和分散曲线施加到观察到的数据,并且获得了下降到200米的S波速度模型。具有低于150米/秒的S波速度的低速层存在于墨西哥盆地中部的70米的深度。似乎H / V光谱中0.25Hz的峰值频率是由于这种浅低速层。

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