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Sedimentary break significance between the Tectosedimentary Units IV2 and N3 in the central part of the Ebro Basin

dc.contributor.authorArenas Abad, Concepción
dc.contributor.authorPardo, Gonzalo
dc.date.accessioned2020-06-03T09:01:12Z
dc.date.available2020-06-03T09:01:12Z
dc.date.issued1990
dc.identifier.urihttp://hdl.handle.net/10272/18132
dc.description.abstractIn the Alcubierre Sierra, the sedimentary break between the Tectosedimentary Units N2 (middle and upper Aragonian) and IV3 (upper Aragonian-Val/esian) represents an important paleogeographic change, related to the diastrophic activity in the northern margin of the Ebro Basin: the expansive lacustrine sedimentation of the TSU IV2 is clearly replaced by alluvial deposits of the TSU N3. This boundary implies a period of subaerial exposition with erosion. A tectonic instability phase in relation to this boundary is shown by a North-South synsedimentary fault system, and small structures such as cracks an slumpses_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSpaines_ES
dc.subject.otherEbro Basines_ES
dc.subject.otherMiddle Aragonan-Vallesianes_ES
dc.subject.otherSedimentary breakes_ES
dc.subject.otherSedimentary structureses_ES
dc.subject.otherSynsedimentary Aectonicses_ES
dc.titleSignificado de la ruptura entre las Unidades Tectosedimentarias N2 y N3 en el centro de la Cuenca del Ebroes_ES
dc.titleSedimentary break significance between the Tectosedimentary Units IV2 and N3 in the central part of the Ebro Basineng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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