Seismic Characterization of Hypogenic Karst Systems Associated with Deep Hydrothermal Fluids in the Middle-Lower Ordovician Yingshan Formation of the Shunnan Area, Tarim Basin, NW China

Figure 9

Relationships of the sedimentary facies and hypogenic karst systems of the upper and lower part of the Yingshan Formation, showing well coupling between the distribution of intraplatform shoals and the development of hypogenic karst systems.