The Impact of Microearthquakes Induced by Reservoir Water Level Rise on Stability of Rock Slope

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/sv/volume-2016/7583108/figures/7583108.fig.0017a.svgz" name="7583108.fig.0017a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Final nephogram of shear strain increments</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/sv/volume-2016/7583108/figures/7583108.fig.0017b.svgz" name="7583108.fig.0017b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Final nephogram of shear strain rates</td></tr></table>

<div>Nephogram of shear strain increments and shear strain rates of the slope after five earthquakes.</div>

Shock and Vibration

fig17

Figure 17

Figure 17: The Impact of Microearthquakes Induced by Reservoir Water Level Rise on Stability of Rock Slope 