Existencia de una plataforma carbonatada del Albiense Superior entre materiales terrígenos de mar somero (Karrantza-Trucíos, Bizkaia)

dc.contributor.authorLópez Horgue, Mikel A.
dc.contributor.authorAranburu Artano, Arantza
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2017-11-06T12:52:59Z
dc.date.available2017-11-06T12:52:59Z
dc.date.issued1992
dc.description.abstractFacies analysis and distribution in the Karrantza and Trucfos Valleys have allowed a detailed correlation of Upper Albian series. A new carbonate platform belonging to the Urgonian Complex is described and correlated with siliciclastic platform sequences of Upper Albian (Hysteroceratian) age. The stationary platform margin shows no signs of steep slopes and was surrounded by a shallow basin dominated by siliciclastics derived from a broad deltaic systemes_ES
dc.identifier.urihttp://hdl.handle.net/10272/14124
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 platform-basines_ES
dc.subject.otherUpper Albianes_ES
dc.subject.otherStratigraphyes_ES
dc.subject.otherKarrantza-Trucioses_ES
dc.titleExistencia de una plataforma carbonatada del Albiense Superior entre materiales terrígenos de mar somero (Karrantza-Trucíos, Bizkaia)es_ES
dc.titleFirst report of the Sopeña carbonate platform correlated with shallow marine siliciclastic sequences (Upper Albian, Urgonian Complex, Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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