Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/34447
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dc.contributor.authorSáez, Alberto-
dc.contributor.authorCabrera, Lluís-
dc.date.accessioned2013-04-04T15:43:46Z-
dc.date.available2013-04-04T15:43:46Z-
dc.date.issued1994-
dc.identifier.issn0213-683X-
dc.identifier.urihttp://hdl.handle.net/2445/34447-
dc.description.abstractThe lacustrine and swampy sequences recorded in the As Pontes basin are rather diverse in terms of facies and sequential arrangement, depending on the considered basin zone. Since these sequences developed synchronously and very close, the paleoclimate conditions had to be similar and the observed differences must be attributed to the tectonic influence.-
dc.format.extent4 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isospa-
dc.publisherSociedad Geológica de España-
dc.relation.ispartofGeogaceta, 1994, vol. 15, p. 59-62-
dc.rights(c) Sociedad Geológica de España, 1994-
dc.subject.classificationSediments lacustres-
dc.subject.classificationCenozoic-
dc.subject.classificationGalícia-
dc.subject.otherLake sediments-
dc.subject.otherCenozoic-
dc.subject.otherGalicia-
dc.titleSedimentación lacustre en la Cuenca Cenozoica de As Pontes (A Coruña)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec081389-
dc.date.updated2013-04-04T15:43:46Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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