Quantifying and Modeling Curved Thrust Fault-propagation Folds at Different Scales

This supporting information provides the all possible model parameters combinations generated by the three structural inversions in the text ( Supplementary Table S1 ), and the uninterpreted outcrop cross section and seismic reflection profiles (Figures S1 to S4). Supplementary Table S1. Model parameters for inverse trishear modelling of the three contractional structures at different scales (fold simulation, field fold outcrop, and New Zealand deepwater fold). Figure S1. An uninterpreted field fold outcrop. See the interpreted section in Figure 4a. Figure S2. Uninterpreted seismic reflection profile A-A`. See the interpreted section in Figure 4a. Figure S3. Uninterpreted seismic reflection profile of PEG-09. See the interpreted section in Figure 6a. Figure S4. Uninterpreted seismic reflection profile of the New Zealand deepwater fold. See the interpreted section in Figure 7b.