Fracture Failure Characteristics of Jointed Sandstone under Uniaxial Compression

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8812522/figures/8812522.fig.0010a.svgz" name="8812522.fig.0010a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>At the first fracture</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8812522/figures/8812522.fig.0010b.svgz" name="8812522.fig.0010b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>At the peak point</td></tr></table>

<div>The fractal dimension of the sandstone surface fracture distribution in zone I.</div>

Geofluids

fig10

Figure 10

Figure 10: Fracture Failure Characteristics of Jointed Sandstone under Uniaxial Compression 