La falla de Ubierna (margen SO de la cuenca Cantábrica)
The Ubierna fault (S. W. margin of the Cantabrian basin)
PublisherSociedad Geológica de España
AbstractThe Ubierna fault is a major structure in the southern margin of the Cantabrian Basin. It controlled the subsidence during the intra-Mesozoic extensional event allow ing the deposit of progressively to the north thicker syn-rift Upper Jurassic-Lower Cretaceous sediments in the Polients trough. Later it was inverted as a reverse fault during the main Tertiary compression changing to a strike-slip behaviour in the latest compressive movements.
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