“…If the lower crust has been subjected to high pressures in a convergent orogen, this would lead to the formation of eclogites, creating a density instability (Elkins-Tanton, 2005;Xu et al, 2012;Zhang et al, 2012a,b,c;Gao et al, 2004), and triggering lower crustal delamination or the convective removal of the eclogitic lower crust (Kay and Kay, 1993;Vlaar et al, 1994;van Thienen et al, 2004). Several seismic studies have illustrated abnormally low velocities for the Tibetan lower crust (Sapin and Hirn, 1997;Cotte et al, 1999;Zhao et al, 1996), precluding the presence of any eclogite (Schulte-Pelkum et al, 2005), which suggests that the lower crust might have been delaminated.…”