Characteristics of Fracture Propagation Induced by Supercritical CO<sub>2</sub> in Inter-Salt-Shale Reservoir

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2019/7132843/figures/7132843.fig.0010a.svgz" name="7132843.fig.0010a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Main fracture induced by SC-CO<sub>2</sub></td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2019/7132843/figures/7132843.fig.0010b.svgz" name="7132843.fig.0010b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Opening natural fracture</td></tr></table>

<div>The morphology of hydraulic fractures on the side surface of the shale specimen.</div>

Geofluids

fig10

Figure 10

Figure 10: Characteristics of Fracture Propagation Induced by Supercritical CO<sub>2</sub> in Inter-Salt-Shale Reservoir 

Geofluids

Characteristics of Fracture Propagation Induced by Supercritical CO2 in Inter-Salt-Shale Reservoir

Figure 10

Characteristics of Fracture Propagation Induced by Supercritical CO₂ in Inter-Salt-Shale Reservoir