Supplemental Material: Structural styles and kinematic evolution of the Front Ranges of the Southern Canadian Rockies

Included in the supplement are details of how we calculated the error for the data presented in our scatterplot, along with seven additional figures. One is additional examples of our binning and fold analysis procedure and the results on three cross sections (m–m′ [51.06467°N, 115.586°W], [51.08187°N, 115.554°W]), n–n′ [50.92633°N, 115.132°W], [50.94936°N, 115.089°W], and o–o′ [51.05612°N, 115.446°W], [51.09349°N, 115.377°W]); palimpsestic restorations of our regional cross sections; high-resolution plates of our compiled geologic maps and associated cross sections; a map of our study area highlighting the bounds of maps we used to create our compiled map; a map of our study area detailing the bounds of our various digital elevation models; an example of our dynamic binning process from the data shown in Figure 5; regional cross sections with strike and dip data projected from 1 km away; and a comparison between different data collection methods. The remotely acquired strike and dip data are available on StraboSpot (https://strabospot.org/). Any GIS files needed to construct any of our geologic map figures in this study are available by emailing the corresponding author.