Reconstruction of the Cenozoic History of Hydrocarbon Fluids from Rifting Stage to Passive Continental Margin Stage in the Huizhou Sag, the Pearl River Mouth Basin

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/4358985/figures/4358985.fig.0023a.svgz" name="4358985.fig.0023a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Present day</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/4358985/figures/4358985.fig.0023b.svgz" name="4358985.fig.0023b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>5.3 Ma</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/4358985/figures/4358985.fig.0023c.svgz" name="4358985.fig.0023c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>10.0 Ma</td></tr><tr class="fig-image" id="d"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/4358985/figures/4358985.fig.0023d.svgz" name="4358985.fig.0023d" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(d) </b>16.0 Ma</td></tr></table>

<div>Dominant hydrocarbon fluid pathway and accumulation model of the Eocene source rocks during postrift and block faulting stage in the Huizhou Sag (the locations of three wells and profile BB′ are shown in Figure <a href="../fig1/">1</a>).</div>

Geofluids

fig23

Figure 23

Figure 23: Reconstruction of the Cenozoic History of Hydrocarbon Fluids from Rifting Stage to Passive Continental Margin Stage in the Huizhou Sag, the Pearl River Mouth Basin 

Figure 23 | Reconstruction of the Cenozoic History of Hydrocarbon Fluids from Rifting Stage to Passive Continental Margin Stage in the Huizhou Sag, the Pearl River Mouth Basin 