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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.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.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
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

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Atribución-NoComercial-SinDerivadas 3.0 España
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