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Shallow-to-deep shear wave velocity profiling by surface waves in complex ground for enhanced seismic microzonation of Las Vegas, Nevada

机译:利用内表面波在复杂地面中的浅至深剪切波速度剖面,以增强内华达州拉斯维加斯的地震微区

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摘要

Shear-wave velocity (VS) profiles were developed using the spectral analysis of Rayleigh-type surface waves (SASW) method for 12 sites in the Las Vegas Valley, Nevada, an urban area that is situated on a deep alluvium-filled basin. The objective of the study was to develop VS profiles to depths of 100 m or deeper to support earthquake site response analyses. To that end, a "minivib" Vibroseis was used in conjunction with an instrumented hammer source, allowing development of deep VS profiles, while also maintaining resolution at shallow depths. The results from optimization by linearized inversion compared well with those from simulated annealing followed by linearized inversion. Data from one site known to have a shallow, high-velocity inclusion were analyzed with the benefit of this independent information, which permitted the depth of the inclusion to be estimated closely. Overall, the VS profiles obtained are consistent with an existing earthquake microzonation of the Valley.
机译:使用瑞利型表面波(SASW)方法的光谱分析,在内华达州拉斯维加斯山谷(位于深冲积盆地中的市区)的12个站点开发了横波速度(VS)剖面。该研究的目的是将VS剖面扩展至100 m或更深,以支持地震现场响应分析。为此,将“ minivib”弧菌与仪器化的锤击声源结合使用,可以产生深VS轮廓,同时还可以在浅深度保持分辨率。通过线性化反演进行优化的结果与通过模拟退火然后进行线性化反演进行优化的结果相比较。利用这一独立信息的优势,分析了一个已知具有浅层高速夹杂物的站点的数据,从而可以精确估计夹杂物的深度。总体而言,获得的VS剖面与山谷现有的地震微区带一致。

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  • 来源
    《Soil Dynamics and Earthquake Engineering》 |2013年第1期|168-182|共15页
  • 作者单位

    Stanley Consultants Inc. 5820 S. Eastern Ave Suite 200 Las Vegas NV 89119 USA;

    Department of Civil & Environmental Engineering and Construction Applied Geophysics Center University of Nevada Las Vegas 4505 S. Maryland Pkwy. Las Vegas NV 89154-4015 USA;

    Ion Geophysical 2105 City West Blvd. Suite 900 Houston TX 77042 USA;

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