“…3.10–3.06, 2.92, 2.4–2.2, and 1.96–1.90 Ga) (Cui et al, 2019, 2020, 2021; Yang et al, 2023) and Phan Si Pan complexes (ca. 2.95, 2.85–2.77, 2.33–2.26, 2.1, and 1.85–1.75 Ga) (Zhao et al, 2019, 2020, 2023a, 2023b). Therefore, the Yangtze Craton possesses a comprehensive record of geological evolution from the Precambrian Archean to the Neoproterozoic (Figure 1b).…”