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SEISMIC MICROZONING STUDY IN BARQUISIMETO, VENEZUELA

机译:Barquisimeto,委内瑞拉的地震微微钟研究

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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:在1998年至2000年期间,在Barquisimeto进行了微局和地震折射调查,用于评估地面振动参数。来自H / V分析的主要时间在0.2至1.1秒之间变化,值在东部0.2和0.5秒之间,其中浅表P波速度范围在1.000和2.000米/ s之间,对应于外包分子。此外,主要的时期增加到0.5和0.8秒之间的平均值,对应于沉积盖的厚度增加。从地震折射测量和岩土钻井分析,特征在镇中心延续至15米,厚度向西方厚度增加。沉积物显示出刚性粘土与砂和砾石的嵌入,S波速度范围为400至600米/秒。

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