Oblique Incidence of Seismic Wave Reflecting Two Components of Design Ground Motion

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/sv/volume-2018/4127031/figures/4127031.fig.0016a.svgz" name="4127031.fig.0016a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Horizontal</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/sv/volume-2018/4127031/figures/4127031.fig.0016b.svgz" name="4127031.fig.0016b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Vertical</td></tr></table>

<div>Acceleration spectrums of Taft earthquake: (a) horizontal and (b) vertical.</div>

Shock and Vibration

fig16

Figure 16

Figure 16: Oblique Incidence of Seismic Wave Reflecting Two Components of Design Ground Motion 