El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica

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dc.contributor.authorLiesa, Carlos L.
dc.contributor.authorCortés Gracia, A. L.
dc.contributor.authorSoria, Ana Rosa
dc.date.accessioned2015-05-11T08:38:10Z
dc.date.available2015-05-11T08:38:10Z
dc.date.issued1997
dc.description.abstractThe 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 anticlineen_US
dc.identifier.urihttp://hdl.handle.net/10272/10540
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.otherNormal faulten_US
dc.subject.otherFolden_US
dc.subject.otherThrusten_US
dc.subject.otherInversion tectonicsen_US
dc.subject.otherCretaceousen_US
dc.subject.otherTertiaryen_US
dc.titleEl anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácicaen_US
dc.titleThe Muel-Jaulín anticline and its relation to the Cretaceous extensioneng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 22, (1997)