Supplemental Material: Late Cretaceous upper-crustal thermal structure of the Sevier hinterland: Implications for the geodynamics of the Nevadaplano

Figure 7. Compilation of cross sections across east-central Nevada and western Utah (1:200,000 scale) with deformed cross sections in the top row (A) and restored cross sections in the bottom row (B). Translucent areas represent eroded rock above the modern surface (deformed cross sections) and above the Paleogene unconformity (restored cross sections).