Significado de la ruptura entre las Unidades Tectosedimentarias N2 y N3 en el centro de la Cuenca del Ebro
Sedimentary break significance between the Tectosedimentary Units IV2 and N3 in the central part of the Ebro Basin
dc.contributor.author | Arenas Abad, Concepción | |
dc.contributor.author | Pardo, Gonzalo | |
dc.date.accessioned | 2020-06-03T09:01:12Z | |
dc.date.available | 2020-06-03T09:01:12Z | |
dc.date.issued | 1990 | |
dc.identifier.uri | http://hdl.handle.net/10272/18132 | |
dc.description.abstract | In 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 slumps | es_ES |
dc.language.iso | spa | es_ES |
dc.publisher | Sociedad Geológica de España | es_ES |
dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
dc.subject.other | Spain | es_ES |
dc.subject.other | Ebro Basin | es_ES |
dc.subject.other | Middle Aragonan-Vallesian | es_ES |
dc.subject.other | Sedimentary break | es_ES |
dc.subject.other | Sedimentary structures | es_ES |
dc.subject.other | Synsedimentary Aectonics | es_ES |
dc.title | Significado de la ruptura entre las Unidades Tectosedimentarias N2 y N3 en el centro de la Cuenca del Ebro | es_ES |
dc.title | Sedimentary break significance between the Tectosedimentary Units IV2 and N3 in the central part of the Ebro Basin | eng |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | es_ES |