RT Journal Article
T1 El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica
T1 The Muel-Jaulín anticline and its relation to the Cretaceous extension
A1 Liesa, Carlos L.
A1 Cortés Gracia, A. L.
A1 Soria, Ana Rosa
AB The Muel-Jaulin region shows structures related to the Lower Cretaceous extension and the Tertiary compression respectively. Cretaceous normal faults constitute the northern border of the Aguilôn Cretaceous basin, appearing Lower Cretaceous deposits (Villanueva de Huerva Fm.) to the South. During the Tertiary compression, minor normal faults were reactivated and folded. Main faults limiting the Cretaceous basin are slightly reactivated and they are responsible for the nucléation of the Muel-Jaulin anticline
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10540
UL http://hdl.handle.net/10272/10540
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026