“…Recent studies have also identified Jurassic (191–159 Ma; Table S4 in Supporting Information ) Neo‐Tethyan ophiolites formed at (ultra)slow‐spreading ocean basins, which are mainly located at the Bangong–Nujiang and Shiquanhe–Yunzhug–Namco sutures in central Tibet (Figure 8; e.g., X. N. Li et al., 2023; Tang et al., 2021; B. C. Zhang et al., 2022; W. Q. Zhang, Liu, Liu, Zhang, et al., 2022), although some researchers defined these ophiolites as belonging to the Meso‐Tethyan orogen (e.g., Metcalfe, 2006; Zhu et al., 2013). These ophiolites are characterized by the occurrence of diabase dikes in the mantle and lower crust (X. N. Li et al., 2023; Tang et al., 2021; W. Q. Zhang, Liu, Liu, Zhang, et al., 2022), ophicalcites containing fault‐breccias of mantle peridotites (B. C. Zhang et al., 2022), and extrusive lavas directly overlying serpentinized mantle peridotites (Tang et al., 2021). Notably, fossil oceanic core complexes have also been identified in these ophiolites (e.g., B. C. Zhang et al., 2022; W. Q. Zhang, Liu, Liu, Zhang, et al., 2022).…”