Un nivel de concentracjon de briozoos en el Cuisiense inferior ; de Esdolomada (Formacion Murillo, Valle del Isabena)

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dc.contributor.authorReguant, Salvador
dc.date.accessioned2015-04-14T10:21:30Z
dc.date.available2015-04-14T10:21:30Z
dc.date.issued1997
dc.description.abstractThe presence of a condensation bed, consisting of a dense lumachellic marly limestone with a nearly monospecific bryozoan (Teichopora clayata Gregory) is indicative of a change in tendency from transgressive to regressive within the transgressive interval constituting the Murillo Formation in the Southcentral Pyreneesen_US
dc.identifier.urihttp://hdl.handle.net/10272/10336
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMurillo Formationen_US
dc.subject.otherLower Cuisianen_US
dc.subject.otherCondensation beden_US
dc.subject.otherBryozoansen_US
dc.subject.otherTransgressive-regressive changeen_US
dc.titleUn nivel de concentracjon de briozoos en el Cuisiense inferior ; de Esdolomada (Formacion Murillo, Valle del Isabena)en_US
dc.titleA bryozoan concentration bed at Esdolomada lower Cuisian (Murillo Formation, Isabena)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 24, (1997)