Evidencias de actividad diapírica sobre las unidades deposicionales del Maastrichtiense en la zona de Laño (Sur de Vitoria, cuenca Vasco-Cantábrica)

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dc.contributor.authorGómez Alday, Juan José
dc.contributor.authorGarcía Garmilla, Francisco
dc.contributor.authorElorza, Javier
dc.date.accessioned2017-07-19T11:04:04Z
dc.date.available2017-07-19T11:04:04Z
dc.date.issued1994
dc.description.abstractThe Laño quarry, situated near Vitoria in the south limb of the Miranda-Treviñ o Synclin orium , show san interesting section of Maastrichtian rocks which were re deposited in a variety of environments, such as marine, transitional and continental settings. These were directly influenced by the Pañacerrada diapir uplift as reflected by the numerous unconformities observed and their progressive relief towards the westes_ES
dc.identifier.urihttp://hdl.handle.net/10272/13944
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.otherMiranda-Treviño synclinales_ES
dc.subject.otherMaastrichtianes_ES
dc.subject.otherDepositional systemses_ES
dc.subject.otherSynsedimentary diapiric activityes_ES
dc.titleEvidencias de actividad diapírica sobre las unidades deposicionales del Maastrichtiense en la zona de Laño (Sur de Vitoria, cuenca Vasco-Cantábrica)es_ES
dc.titleEvidence of diapiric activity upon Maastrichtian depositional units in Laño (South of Vitoria, Basque-Cantabrian basin)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 16, (1994)