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SEISMIC MICROZONING STUDY IN BARQUISIMETO,VENEZUELA

机译:委内瑞拉巴基西摩的地震微区化研究

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Between 1998 and 2000, microtremor and seismic refraction surveys were carried out in Barquisimeto for the evaluation of ground shaking parameters. The predominant periods derived from H/V analysis vary between 0.2 to 1.1 s, with the values varying between 0.2 and 0.5 s in the east, where superficial P-wave velocities range between 1.000 and 2.000 m/s, corresponding to outcropping schists. Further to the west, predominant periods increase to average values between 0.5 and 0.8 s, corresponding to an increasing thickness of the sedimentary cover. From analysis of seismic refraction measurements and geotechnical drillings, characteristics were derived down to 15 m in the center of the town, with increasing thickness to the west. The sediments show an intercalation of stiff clay with sand and gravel, and the S- wave velocities range between 400 and 600 m/s.
机译:1998年至2000年,在Barquisimeto进行了微震和地震折射调查,以评估地震动参数。 H / V分析得出的主要周期在0.2到1.1 s之间变化,东部的变化值在0.2到0.5 s之间变化,东部的表面P波速度范围在1.000和2.000 m / s之间,对应于露片。再往西,主要时段增加到0.5到0.8 s之间的平均值,这与沉积物覆盖层的厚度增加相对应。通过对地震折射测量结果和岩土钻探的分析,得出了镇中心低至15 m处的特征,并且随着西部厚度的增加而增加。沉积物显示出硬质粘土与沙子和砾石之间的夹层,S波速度范围为400至600 m / s。

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