Significado de la discordancia de Mediano en relación con las estructuras adyacentes (Eoceno, Pirineo Central)

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dc.contributor.authorTeixell, Antonio
dc.contributor.authorBarnolas, Antonio
dc.date.accessioned2017-05-29T11:08:24Z
dc.date.available2017-05-29T11:08:24Z
dc.date.issued1995
dc.description.abstractDetailed mapping in the Mediano anticline and surrounding areas reveals that it grew in interference on a tilted limb of a preexisting triassic-cored dome. The well-known unconformity at Mediano is not related to anticline growth but is a previous regional feature that occurs over a larger zone, being associated to the triassic dome. The use of the unconformity and related onlapping series to model the growth of the Mediano anticline should be taken with cautionen_US
dc.identifier.urihttp://hdl.handle.net/10272/13744
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.otherUnconformityen_US
dc.subject.otherAnticlineen_US
dc.subject.otherSalt domeen_US
dc.subject.otherGrowth foldingen_US
dc.subject.otherMedianoen_US
dc.subject.otherPyreneesen_US
dc.titleSignificado de la discordancia de Mediano en relación con las estructuras adyacentes (Eoceno, Pirineo Central)en_US
dc.titleThe Mediano unconformity: significance and relationships to adjoining structures (Eocene, south central Pyrenees)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)