Geomorphology Characterization of Ica Basin and Its Influence on the Dynamic Response of Soils for Urban Seismic Hazards in Ica, Peru

Figure 3

Dispersion curves (slowness versus frequency) obtained using the - method, which considers circular arrays with radii of 10, 30, 100, and 400 m. Dashed lines indicate reliability ranges and the bars in the curves are associated with the dispersion of slowness for each frequency. The right panels show the dispersion curves for different seismic arrays and the solid black line represents the average.