Variación del patrón de diaclasas a lo largo de la serie neógena de la Sierra de Sigena (Huesca): Posible relación con el campo de esfuerzos y su perturbación

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dc.contributor.authorArlegui, L. E.
dc.date.accessioned2019-06-12T12:44:00Z
dc.date.available2019-06-12T12:44:00Z
dc.date.issued1992
dc.description.abstractNeotectonic joints in the Ebro basin strike uniformly NNW-SSE, perpendicular or nearperpendicular to the direction of <33 in the moment it developed. Within the Sierra de Sigena there are joints with anomalous strikes. They show a vertical evolution becoming more similar to the regional fracture pattern as higher in the slope they appair. In the middle portion of the slope this set coexists with the regional-striking joints We interpret this joint distribution as a consequence of stress deflection caused by major faults in the basament, which shows possible attenuation upwardses_ES
dc.identifier.urihttp://hdl.handle.net/10272/16406
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherJointses_ES
dc.subject.otherStress fieldes_ES
dc.subject.otherDeflectiones_ES
dc.subject.otherHuescaes_ES
dc.subject.otherEbro basines_ES
dc.subject.otherAlpine tectonicses_ES
dc.titleVariación del patrón de diaclasas a lo largo de la serie neógena de la Sierra de Sigena (Huesca): Posible relación con el campo de esfuerzos y su perturbaciónes_ES
dc.titleVariation in the joint pattern along the neogene series of the Sierra de Sigena (Huesca): Possible relationships with the stress Field and its deflectioneng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 12, (1992)