Un sistema de fallas normales sinsedimentarias en las unidades de facies Urgon de Aliaga (Teruel, Cordillera Ibérica)

dc.contributor.authorSimón Gómez, José Luis
dc.contributor.authorLiesa, Carlos L.
dc.contributor.authorSoria, Ana Rosa
dc.date.accessioned2015-04-14T10:30:16Z
dc.date.available2015-04-14T10:30:16Z
dc.date.issued1997
dc.description.abstractSystem 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 anticlineen_US
dc.identifier.urihttp://hdl.handle.net/10272/10337
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherLower Cretaceousen_US
dc.subject.otherSynsedimentary faulten_US
dc.subject.otherNormal faulten_US
dc.subject.otherIberian Chainen_US
dc.titleUn sistema de fallas normales sinsedimentarias en las unidades de facies Urgon de Aliaga (Teruel, Cordillera Ibérica)en_US
dc.titleA synsedimentary normal fault system in the Urgon deposits of Aliaga (Teruel province, Iberian Chain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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