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
Data to make the figures in the manuscript: Slab buckling as a driver for rapid oscillations in plate motion and subduction rate by van der Wiel & Pokorny. The readme explains the .txt files.
The data include zircon U-Pb age of a intermediate dike (Table S1-sample STV01-mendeley), and 39Ar-40Ar thermochronology result of mica quartz phyllite (Table S2-Ar-Ar data-mendeley) from the Gyaca mé
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