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Combination of Active (MASW) and Passive (Microtremor) Source Based Geophysical Approach
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, Near Surface 2008 - 14th EAGE European Meeting of Environmental and Engineering Geophysics, Sep 2008, cp-64-00002
- ISBN: 978-90-73781-56-6
Abstract
The microtremor and the MASW (Multi-channel Analysis of Surface Waves) survey were carried out to determine the shear wave velocity-depth information, resonance frequencies and the depths of the sedimentary layer in the Dinar city, Southwestern of Turkey. The shear-wave velocity profile of the basin sediments was estimated from the inversion of the microtremor horizontal-to-vertical spectrum based on surface waves from seismic noise at each site using a genetic algorithm. The average shear-wave velocities estimated from the multichannel analysis of surface waves experiments were given as constraints in the inversion. A new relationship was derived between the resonance frequency ( ) and thickness ( ) of the overlaying layer, which is given as