“…They also feature wide areas of highly thinned, so-called hyperextended crust with a thickness of less than 10 km, where crust and mantle deformation appears to be tightly coupled Mohn et al, 2014]. Well-studied examples of magma-poor margins comprise the Iberia-Newfoundland conjugates [Hopper et al, 2004;Reston, 2007;Ranero and Perez-Gussinye, 2010;Sutra and Manatschal, 2012], the Central South Atlantic segment [Contrucci et al, 2004;Aslanian et al, 2009;Mohriak and Leroy, 2012], the Australian North West Shelf [Karner and Driscoll, 1999], the eastern Gulf of Aden and the South China Sea [Zhou and Yao, 2009;Franke, 2013].…”