“…1: Laredo and Pondra diapirs (López-Horgue et al, 2010); 2: Poza de la Sal diapir (Quintà et al, 2012); 3: Bakio diapir (Poprawski et al, 2014(Poprawski et al, , 2016; 4: Lasarte sub-basin salt controlled basin (Bodego & Agirrezabala, 2013;Bodego, Iriarte, López-Horgue, & Álvarez, 2018); 5-7: Gaujacq and Ossun diapirs (Canérot et al, 2005); 6: Mauléon basin diapirs (Jammes et al, 2010); 8: Cotiella extensional salt area (McClay et al, 2004); 9: Sopeira and Sant Gervàs diapirs (Saura et al, 2016); 10: Villahermosa del Rio diapir (Canérot, 1991); 11: Parcent diapir (Pedrera et al, 2014); 12: Altea diapir (Pedrera et al, 2014;Martínez del Olmo et al, 2015); 13, 14: Finestrat and Elda diapirs (Martínez del Olmo et al, 2015); 15: Jumilla diapirs (Escosa et al, 2018); 16: Western Betics ; 17, 18: Faro and Albuferia diapirs (Ramos et al, 2016); 19, 20: Santa Cruz and Caldas da Rainha diapirs (Alves et al, 2003;Pena do Reis et al, 2017). Iberian Range AB: Aragoneses Branch; Iberian Range CB: Castillan Branch; PB: Parentis Basin; AB: Asturian Basin; AP: As Pontes Basin; ALZ: Asturoccidental-Leonese Zone; CZ: Cantabric Zone; CM: Cantabrian Mountain; CS: Central System; CCR: Catalan Coastal Range; GB: Guadalquivir Basin unconformities within the Jurassic and Lower Cretaceous successions were traditionally interpreted in terms of syn-rift to post-rift differential subsidence between fault-bounded tectonic domains (Aurell et al, 1992;Campos, Aurell, & Casas, 1996;Guimerà, 1988;Liesa, Soria, Meléndez, & Meléndez, 2006;Roca & Guimerà, 1992;Roca, Guimerà, & Salas, 1994;. The only previously documented examples of halokinesis within the Maestrat Basin are a diapir located in the Penyagolosa block near Villahermosa del Río village and in Lucena del Cid, north of Castelló (Canérot, 1989(Canérot, , 1991Trell, Canérot, & Martín, 1979) (see location in…”