Topographic Effects on the Seismic Response of Trapezoidal Canyons Subjected to Obliquely Incident SV Waves

<div>The (a) horizontal and (b) vertical Fourier amplitudes at the canyon crests for different heights of the canyon and incident angles of SV waves.</div>

Shock and Vibration

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Figure 12

Figure 12: Topographic Effects on the Seismic Response of Trapezoidal Canyons Subjected to Obliquely Incident SV Waves 