Late Neogene lacustrine record and paleogeography in the Quillagua-Llamara basin, Central Andean fore-arc (Northern Chile)

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RECERCAT Principal > Universitat de Barcelona > Dinàmica de la Terra i l'Oceà > Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) > Visualizar documento

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dc.contributor	Universitat de Barcelona
dc.contributor.author	Sáez, Alberto
dc.contributor.author	Cabrera, Lluís
dc.contributor.author	Jensen, A.
dc.contributor.author	Chong, Guillermo
dc.date	2013-04-03T16:45:41Z
dc.date	2013-04-03T16:45:41Z
dc.date	1999
dc.date	2013-04-03T16:45:41Z
dc.identifier.citation	0031-0182
dc.identifier.citation	145794
dc.identifier.uri	http://hdl.handle.net/2445/34428
dc.format	33 p.
dc.format	application/pdf
dc.language.iso	eng
dc.publisher	Elsevier B.V.
dc.relation	Palaeogeography Palaeoclimatology Palaeoecology, 1999, vol. 151, num. 1-3, p. 5-37
dc.rights	(c) Elsevier B.V., 1999
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Sediments lacustres
dc.subject	Neogen
dc.subject	Xile
dc.subject	Andes (Regió)
dc.subject	Lake sediments
dc.subject	Neogene
dc.subject	Chile
dc.subject	Andes Region
dc.title	Late Neogene lacustrine record and paleogeography in the Quillagua-Llamara basin, Central Andean fore-arc (Northern Chile)
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/acceptedVersion
dc.description.abstract	The 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.

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