“…Tomographic approaches using data on the relative traveltime of teleseismic body waves have been used to image upper mantle structures from continental scales (e.g., Argnani et al, ; Biryol et al, ; Schmandt & Lin, ) to regional scales (e.g., Bastow et al, ; Rawlinson & Kennett, ; Schlömer et al, ). This method has been successful in revealing detailed three‐dimensional (3‐D) velocity heterogeneities beneath seismic arrays by taking advantage of individual rays from a common event sharing the same path outside of the region of interest and sampling velocity variations inside the modeled space (Aki et al, ; Lévêque & Masson, ; Thurber, ). This method has provided useful information on unrevealed localized upper mantle structures, for example, in Northeast (NE) Asia (e.g., Chen et al, ; Lei & Zhao, ; Ma et al, ; Zhao et al, ).…”