“…We note here that modal mineralogy in combination with infrared (IR) spectroscopy is helping to strengthen links between meteorites and their parent bodies (Beck et al, 2010McAdam et al, 2015). A significant fraction of C-type asteroids appear to have dehydrated surfaces with spectral features similar to those of the thermally metamorphosed CI-like chondrites (Hiroi et al, 1993(Hiroi et al, , 1996Osawa et al, 2005;Cloutis et al, 2012). The timing and mechanism of the thermal metamorphism remains poorly constrained, although studies of mineral textures (Nakato et al, 2008) and organics (Yabuta et al, 2010;Orthous-Daunay et al, 2013;Quirico et al, 2014) in the heated CM chondrites indicate that the process was short-lived and probably took place on the order of hours to several years.…”