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A carbonate paleohigh-siliciclastic trough system (Gorbea-Artzentales, middle Album, Bizkaia)

dc.contributor.authorGómez Pérez, I.
dc.contributor.authorAranburu Artano, Arantza
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2017-07-24T10:35:50Z
dc.date.available2017-07-24T10:35:50Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/13970
dc.description.abstractDuring the middle Albian, fault block synsedimentary activity induced the formation of a paleohigh (Corbea) and an adjacent sedimentary trough, While (he high was exposed in the subaerial meteoric environment realm, the trough was filled by athick wedge up to 2 km of deeper water siliciclasticses_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.otherAlbianes_ES
dc.subject.otherCarbonate platformes_ES
dc.subject.otherPaleokarstes_ES
dc.subject.otherSillciclastic troughes_ES
dc.subject.otherSinsedimentary faultses_ES
dc.titleUn sistema de paleoalto carbonatado-surco siliciclástico (Gorbea-Artzentales, Albiense medio, Bizkaia)es_ES
dc.titleA carbonate paleohigh-siliciclastic trough system (Gorbea-Artzentales, middle Album, Bizkaia)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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