首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Determination of S-wave velocity structure using microtremors and spac method applied in Thessaloniki (Greece)
Authors:Paschalis Apostolidis  Dimitrios Raptakis  Zafeiria Roumelioti  Kyriazis Pitilakis
Institution:a Department of Civil Engineering, Aristotle University of Thessaloniki, P.O. Box 450, GR-54124, Thessaloniki, Greece;b Department of Geology, Aristotle University of Thessaloniki, P.O. Box 352-1, GR-54124, Thessaloniki, Greece
Abstract:Array measurements of microtremors at 16 sites in the city of Thessaloniki were performed to estimate the Vs velocity of soil formations for site effect analysis. The spatial autocorrelation method was used to determine phase velocity dispersion curves in the frequency range from 0.8–1.5 to 6–7 Hz. A Rayleigh wave inversion technique (stochastic method) was subsequently applied to determine the Vs profiles at all the examined sites. The determination of Vs profiles reached a depth of 320 m. Comparisons with Vs values from cross-hole tests at the same sites proved the reliability of the SPAC method. The accuracy of the Vs profiles, the ability to reach large penetration depths in densely populated urban areas and its low cost compared to conventional geophysical prospecting, make Mictrotremor Exploration Method very attractive and useful for microzonation and site effects studies. An example of its application for the site characterization in Thessaloniki is presented herein.
Keywords:Shear wave velocity  Stationary random functions  Spatial autocorrelation method  Bessel functions  S-wave inversion  Site characterization  2D cross-sections  3D mapping
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号