“…When two continents collide, the tensile stresses between the buoyant continental lithosphere and previously subducted oceanic lithosphere lead to the separation of the oceanic slab from the continental lithosphere (e.g., Davies and von Blanckenburg, 1995;van Hunen and Allen, 2011;von Blanckenburg and Davis, 1995). Slab break-off typically occurs in the early stages of continental collisions (von Blanckenburg and Davis, 1995), and can place important constraints on associated collision dynamics (van Hunen and Allen, 2011). Timing and other details of the Neo-Tethyan slab break-off in the India-Asia collision belt have long been an issue of hot debate (e.g., Chung et al, 2005;Ji et al, 2009Ji et al, , 2012Lee et al, 2009Lee et al, , 2012Wen et al, 2008a;Xu et al, 2008;Zhu et al, 2013).…”