Abstract
Crustal structures of the Central and Eastern Pyrenees are compared with those of the Alps and Carpathians. By analogy, northward subduction/underthrusting in the Central and Eastern Pyrenees is proposed. Southward subduction/underthrusting is found along the North Iberian margin and Western Pyrenees. Hence, a flip—a change in the direction of subduction/underthrusting—is postulated between the Central and Western Pyrenees.
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