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Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/34427
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dc.contributor.authorSáez, Alberto-
dc.contributor.authorInglès i Urpinell, Montserrat-
dc.contributor.authorCabrera, Lluís-
dc.contributor.authorHeras, A. de las-
dc.date.accessioned2013-04-03T16:39:30Z-
dc.date.available2013-04-03T16:39:30Z-
dc.date.issued2003-
dc.identifier.issn0037-0738-
dc.identifier.urihttp://hdl.handle.net/2445/34427-
dc.description.abstractTwo small, alluvial-lacustrine subbasins developed during the early restraining overstep stages of the Oligocene-Miocene As Pontes strike-slip Basin (NW Spain). Later, the basin evolved into a restraining bend stage and an alluvial-swamp-dominated depositional framework developed. The palaeobiological record demonstrates that the Oligocene-Miocene palaeoclimate in NW Spain was subtropical, warm and humid to subhumid.-
dc.format.extent20 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherElsevier B.V.-
dc.relation.ispartofSedimentary Geology, 2003, vol. 159, num. 3-4, p. 305-324-
dc.rights(c) Elsevier B.V., 2003-
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)-
dc.subject.classificationSediments fluvials-
dc.subject.classificationOligocè-
dc.subject.classificationMiocè-
dc.subject.classificationEspanya-
dc.subject.otherRiver sediments-
dc.subject.otherOligocene-
dc.subject.otherMiocene-
dc.subject.otherSpain-
dc.titleTectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain)eng
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/acceptedVersion-
dc.identifier.idgrec508879-
dc.date.updated2013-04-03T16:39:30Z-
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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