Supplemental Material: Cenozoic pure-shear thickening of the northern Tibetan Plateau margin: Implications for diverse plateau uplift mechanisms controlled by convergent obliquity

<p>Figure S1: Compiled geophysical observations across the central segment of the Altyn Tagh fault system, showing the Moho offset by the Altyn Tagh and North Altyn faults. Figure S2: Uninterpreted seismic profiles L1–L4 in the SE Tarim Basin, China, with the locations shown in Figure 2A. Figure S3: Uninterpreted seismic profiles L5–L8 in the SE Tarim Basin, China, with the locations shown in Figure 2A. Figure S4: Published seismic profiles showing southeastward thinning of the Cenozoic strata along the western and eastern segments of the Altyn Tagh fault, with the locations shown in Figure 1A. Table S1: Seismic velocity model of well R1 derived from the vertical seismic velocity profile (VSP) data.</p>