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 inclinations of the canyon and incident angles of SV waves.</div>

Shock and Vibration

fig17

Figure 17

Figure 17: Topographic Effects on the Seismic Response of Trapezoidal Canyons Subjected to Obliquely Incident SV Waves 