The transition from active to passive continental margin of the South China Sea (SCS) is usually inferred to occur in the Late Mesozoic to the Early Cenozoic, however, the specific time and processes
Sample Number: LM 13 Position (#): 18 Area of Graticule Square: 6.400E-07 No. of Crystals: 20 Zeta Factor ±Error: 305.8± 8.4 Rho d (% Relative Error): 1.580E+06 N d: 5057 Mineral: Apatite Glass (U ppm
This .zip file contains Appendix 1a, Appendix 2, and Tables S1 and S2 associated with Amidon, W.H., Kylander-Clark, A.R.C., Barr, M.N. et al. Pace of passive margin tectonism revealed by U-Pb dating o
