Climate as the great equalizer of continental-scale erosion

The following supporting information contains: The detailed location and age data for the thermochronology used in this study, and their associated publications, paleogeographical reconstructions, bouguer gravity anomaly (crustal thickness) for Central Asia, averaged modern rainfall for Central Asia and paleoclimate simulation methods. <br><br>Table S1. List of samples, latitude, longitude (WGS84), reported age, reported error, associated publication, and thermochronometric method.<br><br><br>Table S2. A complete list of publications used in this study. Publications which did not provide precise latitude and longitude measurements are noted. Thermochronometric ages can be found in Table S1.<br><br><i>For inquiries regarding the contents of this dataset, please contact the Corresponding Author listed in the README.txt file. Administrative inquiries (e.g., removal requests, trouble downloading, etc.) can be directed to [e-mail]</i>