RT Journal Article
T1 Un sistema de fallas normales sinsedimentarias en las unidades de facies Urgon de Aliaga (Teruel, Cordillera Ibérica)
T1 A synsedimentary normal fault system in the Urgon deposits of Aliaga (Teruel province, Iberian Chain)
A1 Simón Gómez, José Luis
A1 Liesa, Carlos L.
A1 Soria, Ana Rosa
AB System of conjugate, E-W to NE-SW striking normal faults is reconstructed from mapping and structural analysis of deformation in the Urgon deposits of the Aliaga region. Those were mainly active during the Aptian age, giving rise to significative changes both in thickness and lithology of the stratigraphical unities. An unconformity found in the Escucha Formation clearly separates syn- and post-rift deposits in the western zone of the studied area. The faults were tilted and folded during the Palaeogene within the Campos-Aliaga anticline
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10337
UL http://hdl.handle.net/10272/10337
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026