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 8

Relationships of paleogeomorphology and hypogenic karst systems of the upper part of the Yingshan Formation, showing belt-shaped distributions at the highlands of the margin of intraplatform along the SN4 fault zone.