@article{10272/10540,
year = {1997},
url = {http://hdl.handle.net/10272/10540},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica},
title = {The Muel-Jaulín anticline and its relation to the Cretaceous extension},
author = {Liesa, Carlos L. and Cortés Gracia, A. L. and Soria, Ana Rosa},
}