Extrusion zone of the cardona diapir, located at the Catalan Potash sub-basin (Ebro Basin, NE Iberia). Halite, anhydrite and Sylvite interlayers are strongly folded as a result of the salt ductile flow during diapirism. Evaporite layers exhibiti thin intercalations of claystone and marlstone.
Extrusion zone of the cardona diapir, located at the Catalan Potash sub-basin (Ebro Basin, NE Iberia). Halite, anhydrite and Sylvite interlayers are strongly folded as a result of the salt ductile flow during diapirism. Evaporite layers exhibiti thin intercalations of claystone and marlstone.