“…Diverse methods have been applied to quantify denudation rates, including landscape morphometry, heavy-mineral analyses, bulk-sediment geochemistry, isotope fingerprints of detrital K-feldspar, cosmogenic isotopic tracers, and detrital-zircon geochronology (Chappell et al, 2006;Jie et al, 2007;Yang et al, 2009Yang et al, , 2012Jia et al, 2010b;He et al, 2013aHe et al, , 2014Zhang et al, 2014). Erosion patterns inferred from these different approaches, however, diverge widely.…”