RT Journal Article
T1 La falla de Ubierna (margen SO de la cuenca Cantábrica)
T1 The Ubierna fault (S. W. margin of the Cantabrian basin)
A1 Hernaiz Huerta, Pedro P.
AB 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.
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13952
UL http://hdl.handle.net/10272/13952
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026