Research Article

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 7

Seismic dip section showing individual string-beads-like seismic reflections of epigenic karst systems in the lower part of the Yingshan Formation, which developed near the base and top of sequence boundary in the topographic highland and lowland, respectively.