“…Anisotropy measured by shear wave splitting (SWS) (Deng et al, 2017;Eakin et al, 2014Eakin et al, , 2015Long et al, 2016;Lynner & Beck, 2020;Polet et al, 2000;Reiss et al, 2018) has shown evidence for subduction segments with contrasting mantle geodynamics below two different ridge systems. Good coverage of SWS observation from dense seismic arrays in South America, where the Nazca and Iquique ridges subduct (Figure 1b), allows us to improve the quality of teleseismic tomography by incorporating anisotropy and thus to clarify mantle geodynamic processes (e.g., Bezada et al, 2016;Huang et al, 2019;Lee et al, 2021Lee et al, , 2022Wang & Zhao, 2012;Zhao et al, 2016). In particular, we can investigate whether SSLAs on isotropic velocity models can be explained by anisotropic structure.…”