Stability Monitoring and Deformation Laws of the Yuanjue Cave in the Influence Zone of the Unloading Zone

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2021/6696030/figures/6696030.fig.003a.svgz" name="6696030.fig.003a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Section of annular denudation zone</td></tr><tr class="fig-image" id="b"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2021/6696030/figures/6696030.fig.003b.svgz" name="6696030.fig.003b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Distribution of roof water damage types</td></tr><tr class="fig-image" id="c"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2021/6696030/figures/6696030.fig.003c.svgz" name="6696030.fig.003c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Top plate L6 crack denudation groove</td></tr></table>

<div>Water damage and surface erosion on the roof of the Yuanjue Cave.</div>

Geofluids

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Figure 3

Figure 3: Stability Monitoring and Deformation Laws of the Yuanjue Cave in the Influence Zone of the Unloading Zone 