Mantle-driven plate convergence due to slab detachment

Introduction Data_Fig.1: Elevation profile of the Baja California Sur continental margin (Location 1), Southern Costa Rica (Location 2), Chile continental margin (Location 3), Mediterranean-Carpathian region (Location 4), Zagros orogen (Location 5), and Himalayas orogen (Location 6). Data_Fig.2: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. 2. Data_Fig.3: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. 3. Data_Fig.4: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. 4. Data_Fig.5: The data include the global mantle convection modeling results of Conrad et al. (2010). The data from Hu et al. (2024) are available from the corresponding author upon request. Data_Fig.6: The elevation and age of the Himalaya-Tibetan Plateau. Data_Fig.S3: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. S3. Data_Fig.S4: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. S4. Data_Fig.S5: The primary *.prn data and the extracted viscosity, velocity, and elevation data of the models shown in Fig. S5.