On the Freeze-Thaw Instability of an Open Pit Slope Using Three-Dimensional Laser Scanning and Numerical Simulation

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2022/1705985/figures/1705985.fig.007a.svgz" name="1705985.fig.007a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Distribution characteristics of occurrence</td></tr><tr class="fig-image" id="b"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2022/1705985/figures/1705985.fig.007b.svgz" name="1705985.fig.007b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>The result of stereographic projection</td></tr></table>

<div>Occurrence distribution characteristics of the rock mass structural plane after clustering and the result of stereographic projection.</div>

Geofluids

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Figure 7

Figure 7: On the Freeze-Thaw Instability of an Open Pit Slope Using Three-Dimensional Laser Scanning and Numerical Simulation 