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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.