Variability and Main Controlling Factors of Hydrocarbon Migration and Accumulation in the Lower Paleozoic Carbonate Rocks of the Tazhong Uplift, the Tarim Basin, Northwest China

Figure 3

Seismic profile characteristics of thrust faults in the Tazhong Uplift. No. 1 Fault Zone is a basement-involved reverse fault, and No. 10 Fault Zone and the Central Horst Zone are surface detachment thrust faults which fracture down to the Middle Cambrian gypsum-salt rocks. The three thrust faults have different fault displacements, fault widths, and active periods.