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Post-seismic investigations repeatedly indicate that structures having frequencies close to foundation soil frequencies exhibit significantly heavier damages (Caracas 196 [...]
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Data provided by accelerometric networks are important for seismic hazard assessment. They are key to derive Ground Motion Prediction Equations (GMPEs). The correct use o [...]
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The purpose of this study is to obtain a ''reasonable ensemble'' of one dimensional shear wave velocity models that explain an observed surface wave dispersion curve with [...]
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Yutaka Nakamura (1989; [1]) popularized the application of the horizontal-to-vertical spectral ratio (HVSR) analysis of microtremor (ambient noise or vibration) recording [...]
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The InterPacific project (Intercomparison of methods for site parameter and velocity profile characterization) aims to assess the reliability of seismic site characteriza [...]
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Spatial variability of earthquake ground motion (SVEGM) refers to the differences in amplitude and phase between recordings of the same earthquake at different locations. [...]
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It has been observed repeatedly in the post-earthquake investigations that buildings having frequency similar to soil frequency (coming from H/V for example) exhibit sign [...]
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The city of Grenoble in the French Alps is settled on top of hundreds of meters of post-glacial sediments which cause ground motion to be significantly increased in terms [...]
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In order to understand and predict earthquake ground motions at high frequencies, it is necessary to evaluate a superficial S-wave velocity structure. In the Grenoble bas [...]
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Tehran, capital of Iran, is under the threat of large magnitude earthquakes (above 7) located on very near faults. Previous studies on the effect of local surface geology [...]
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