“…With the dawn of the XXI century, techniques such as geochronology and lowtemperature thermochronology have become more precise and modeling approaches have become more sophisticated, providing higher resolution timing constraints on tectonic events and episodes of exhumational cooling in the upper crust. In recent years, pioneering studies (Figures 2, 3) have highlighted the role of low temperature thermochronology (Mora, 2015;Mora et al 2010aMora et al , 2013aMora et al , 2013bMora et al , 2015aMora et al , 2015bParra et al, 2009aParra et al, , 2009bParra et al, , 2010Parra et al, , 2012Saylor et al, 2012a;Spikings et al, 2000Spikings et al, , 2001Villagómez et al, 2011aVillagómez et al, , 2011b and detrital geochronology (Caballero et al, 2013a(Caballero et al, , 2013bHorton et al, 2010aHorton et al, , 2010bHorton et al, , 2015Nie et al, 2010Nie et al, , 2012Saylor et al, 2011Saylor et al, , 2012bSaylor et al, , 2013Silva et al, 2013) in the Cretaceous to Cenozoic evolution of the northern Andes. Paleoelevation techniques have also become more sophisticated, but their use has been limited in the tropical northern Andes (Anderson et al, 2015) relative to their use in the arid central Andes (Garzione et al, 2017;Saylor & Horton, 2014).…”