@article{10272/13952,
year = {1994},
url = {http://hdl.handle.net/10272/13952},
abstract = {The 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.},
publisher = {Sociedad Geológica de España},
title = {La falla de Ubierna (margen SO de la cuenca Cantábrica)},
title = {The Ubierna fault (S. W. margin of the Cantabrian basin)},
author = {Hernaiz Huerta, Pedro P.},
}