Study on Propagation Behaviors of Hydraulic Fracture Network in Tight Sandstone Formation with Closed Cemented Natural Fractures

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8833324/figures/8833324.fig.003a.svgz" name="8833324.fig.003a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Geometry of HF on the interface between L-A and L-B</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8833324/figures/8833324.fig.003b.svgz" name="8833324.fig.003b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Geometry of HF reflected by AE signal</td></tr></table>

<div>Hydraulic fracture morphology observed in the cross-section of the fractured specimen and reflected by AE data.</div>

Geofluids

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Figure 3

Figure 3: Study on Propagation Behaviors of Hydraulic Fracture Network in Tight Sandstone Formation with Closed Cemented Natural Fractures 