Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/34428
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dc.contributor.authorSáez, Alberto-
dc.contributor.authorCabrera, Lluís-
dc.contributor.authorJensen, A.-
dc.contributor.authorChong, Guillermo-
dc.date.accessioned2013-04-03T16:45:41Z-
dc.date.available2013-04-03T16:45:41Z-
dc.date.issued1999-
dc.identifier.issn0031-0182-
dc.identifier.urihttp://hdl.handle.net/2445/34428-
dc.description.abstractThe Cenozoic Quillagua-Llamara basin (northern Chile, Central Andes) is an asymmetrical, intramassif fore-arc basin with a relatively wide northern sector separated from a narrower southward extension by a basement threshold. The north- ern sector was characterised by a noticeable Oligocene?-late Neogene alluvial-fan and lacustrine dominated deposition which resulted in sequences up to 900 m thick, whereas the southern sector was often a bypass zone with thinner fluvial and lacustrine sediment accumulation.-
dc.format.extent33 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherElsevier B.V.-
dc.relation.ispartofPalaeogeography Palaeoclimatology Palaeoecology, 1999, vol. 151, num. 1-3, p. 5-37-
dc.rights(c) Elsevier B.V., 1999-
dc.subject.classificationSediments lacustres-
dc.subject.classificationNeogen-
dc.subject.classificationXile-
dc.subject.classificationAndes (Regió)-
dc.subject.otherLake sediments-
dc.subject.otherNeogene-
dc.subject.otherChile-
dc.subject.otherAndes Region-
dc.titleLate Neogene lacustrine record and paleogeography in the Quillagua-Llamara basin, Central Andean fore-arc (Northern Chile)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/acceptedVersion-
dc.identifier.idgrec145794-
dc.date.updated2013-04-03T16:45:41Z-
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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