“…Mineral chemistry and bulk-rock geochemistry, especially isotopic geochemistry, have also proven useful in provenance studies (e.g., Krippner et al, 2014;Li et al, 2015;Weldeab et al, 2002;Zahid and Barbeau, 2013). In recent years, sediment provenance studies have been revolutionized by technological developments enabling single-grain radiometric dating of some components of the detrital grain population, for example U-Pb dating of zircon (Bertotti et al, 2014;Jiang et al, 2015;Morton et al, 2008;Shao et al, 2016;Xu et al, 2016;Yao et al, 2014) and rutile (Bracciali et al, 2013), and Ar-Ar dating of hornblende (Hemming et al, 2000), mica (Haines et al, 2004;Van Hoang et al, 2010), and bulk sediments (Van Laningham and Mark, 2011).…”