Supplemental Material: Intracontinental convergence accommodated by underthrustingof Tarim Basin beneath central Tian Shan, Central Asia: Insights from Cenozoic upper crust deformation across the western Kepingtage fold-and-thrust belt in the northern Tarim Basin

Figure S1: The original uninterpreted seismic reflection profile of Line B–B′ and related observations, with its location shown in Figure 1. Figure S2: The original uninterpreted seismic reflection profile of Line C–C′ and related observations, with its location shown in Figure 1. Figure S3: The original uninterpreted seismic reflection profile of Line D–D′ and related observations, with its location shown in Figure 1. Figure S4: The original uninterpreted seismic reflection profile of Line E–E′ and related observations, with its location shown in Figure 1.