Sáez, AlbertoCabrera, LluísJensen, A.Chong, Guillermo2013-04-032013-04-0319990031-0182https://hdl.handle.net/2445/34428The 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.33 p.application/pdfeng(c) Elsevier B.V., 1999Sediments lacustresNeogenXileAndes (Regió)Lake sedimentsNeogeneChileAndes Regioninfo:eu-repo/semantics/article1457942013-04-03info:eu-repo/semantics/openAccess