El modelo de plataforma carbonatada del Albiense superior de Sopeña (Karrantza, Bizkaia)

dc.contributor.authorLópez Horgue, Mikel A.
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.date.accessioned2017-07-19T08:37:10Z
dc.date.available2017-07-19T08:37:10Z
dc.date.issued1994
dc.description.abstractA first detailed analysis of the UpperAlbian sequence of the Sopeña area, Karrantza valley (Bizkaia), is documented. E-W and N-S cross sections of the Sopeña platform Indicate different types of platform margins adjacent to basinal troughs with siliciclastic deposition. Internally, the Sopeña platform contains at least five sedimentary breaks, probably caused by relative sea-level falls of tectonic origin. A biostratigraphic analysis of the limestones (orbitolinids) gives a confident dating of the inflatumdispar ammonite zoneses_ES
dc.identifier.urihttp://hdl.handle.net/10272/13937
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 platformes_ES
dc.subject.otherUpper Albianes_ES
dc.subject.otherSiliciclastic basines_ES
dc.subject.otherSedimentary breakses_ES
dc.titleEl modelo de plataforma carbonatada del Albiense superior de Sopeña (Karrantza, Bizkaia)es_ES
dc.titleThe Sopeña carbonate platform model. UpperAlbian of Karrantza valley, north Iherían píateeng
dc.typejournal articlees_ES
dspace.entity.typePublication

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