Tectónica sinsedimentaria en un talud carbonatado con resedimentación gravitatoria en masa (Ibarra, Albiense Inferior, Bizkaía)

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dc.contributor.authorGómez Pérez, I.
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2017-11-10T11:44:40Z
dc.date.available2017-11-10T11:44:40Z
dc.date.issued1992
dc.description.abstractThe analysis of fades and thickness distribution in carbonate slope systems of the Albian of Ibarra (Bizkaia) indicates active synsedimentary faulting. E-W extensional faults separate blocks that record tilting and depocenter shifts through time. This local extension occurs associated to major NW-SE strike-slip sinistral movements linke d to the opening of the Bay o f Biscayes_ES
dc.identifier.urihttp://hdl.handle.net/10272/14148
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.otherCarbonate slopees_ES
dc.subject.otherLower Albianes_ES
dc.subject.otherSynsedimentary faultses_ES
dc.subject.otherMegabrecciases_ES
dc.titleTectónica sinsedimentaria en un talud carbonatado con resedimentación gravitatoria en masa (Ibarra, Albiense Inferior, Bizkaía)es_ES
dc.titleSynsedimentary tectonics in a carbonate slope dominated by mass-gravity deposits (Ibarra, Lower Albian, Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 13, (1992)