In the orogen-foreland shortening system, pure-and simple-shear are two common shortening modes in foreland deformation belts. The pure-shear shortening mode is characterized by a vertically quasi-homogeneous thickening of the foreland crust. In contrast, the foreland lithosphere underthrusts beneath the orogen along a low-angle detachment fault in the simple-shear mode. During shortening, crustal-scale deformation in the foreland forms either shallow thin-skinned, or deep thick-skinned tectonics (e.g., Dahlen, 1990;Lacombe & Bellahsen, 2016;Pfiffner, 2017). In the former, the sedimentary cover overlies the almost undeformed basement along a shallow décollement fault, while faults reach down into the basement in the latter. These different foreland deformation patterns (i.e., shortening mode and tectonic style) are generally found in natural orogens, for example, in the Central-Southern Andes (e.g.,