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dc.contributor.authorOlóriz, F.
dc.contributor.authorRodríguez Tovar, F. J.
dc.date.accessioned2019-05-29T11:37:49Z
dc.date.available2019-05-29T11:37:49Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16327
dc.description.abstractIn the Central Prebetic the sediments of Early Kimmeridgian age (Platynota Chron) are represented by rhyth¬mic successions which are make up by marls, marly limestones and limestones. In the context of an integrated research programme and in order to analyze the sedimentary cyclicity It is proved the significance of ichnologic studies to reveal the existence of secondary overprint which determines the location of the boundary in marly- limestone couplets as they are recognizable at the outcropes_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.otherIchnologic studieses_ES
dc.subject.otherRhythmic successionses_ES
dc.subject.otherSecondary overprintes_ES
dc.subject.otherEarly Kimmeridgian (Platynota Chron)es_ES
dc.subject.otherCentral Prebetices_ES
dc.titleContribución del análisis icnológico en la interpretación del origen de la rítmita margoso-calcárea de edad Kimmeridgiense inferior (Zona Platynota) en el Prebético Centrales_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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