Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/34426
Full metadata record
DC FieldValueLanguage
dc.contributor.authorSáez, Alberto-
dc.contributor.authorCabrera, Lluís-
dc.date.accessioned2013-04-03T16:27:03Z-
dc.date.available2013-04-03T16:27:03Z-
dc.date.issued2002-
dc.identifier.issn0037-0746-
dc.identifier.urihttp://hdl.handle.net/2445/34426-
dc.description.abstractA small, closed, lacustrine system developed during the restraining overstep stages of the Oligocene As Pontes strike-slip basin (Spain). The increase in basin accommodation and the headward spread of the drainage, which increased the water input, triggered a change from shallow, holomictic to deeper, meromictic conditions.-
dc.format.extent22 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherInternational Association of Sedimentologists-
dc.relation.ispartofSedimentology, 2002, vol. 49, num. 5, p. 1073-1094-
dc.rights(c) Sáez, Alberto et al., 2002-
dc.subject.classificationSediments lacustres-
dc.subject.classificationEspanya-
dc.subject.otherLake sediments-
dc.subject.otherSpain-
dc.titleSedimentological and palaeohydrological responses to tectonics and climate in a small, closed lacustrine system: Oligocene As Pontes Basin (Spain)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/acceptedVersion-
dc.identifier.idgrec502974-
dc.date.updated2013-04-03T16:27:03Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

Files in This Item:
File Description SizeFormat 
502974.pdf2.55 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.