Sedimentological and palaeohydrological responses to tectonics and climate in a small, closed lacustrine system: Oligocene As Pontes Basin (Spain)

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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.date.updated2013-04-03T16:27:03Z
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.identifier.idgrec502974
dc.identifier.issn0037-0746
dc.identifier.urihttps://hdl.handle.net/2445/34426
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.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)
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

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