“…Low‐temperature thermochronology data have revealed that the eastern TP has undergone rapid exhumation since the late Cenozoic (Godard et al, ; Richardson et al, ; Tan et al, , ; Tian et al, ; E. Wang et al, ). It has been estimated that the LMS was denuded ~7–10 km during the Cenozoic (B. Deng et al, ; Tan et al, ), which resulted in the exposure of Precambrian metasedimentary or igneous rocks (Burchfiel et al, ; S.F. Chen et al, ; Lu et al, ; Yin & Harrison, ).…”