Pena dos Reis, R.Antunes, MiguelPais, J.2015-01-292015-01-292000http://hdl.handle.net/10272/9777Eocene and Oligocene terrestrial sediments of the "Complexo de Benfica", near Lisbon, display different facies associations and two main infill sequences. They are separated by an unconformity. Depositional systems, controls and chronological boundaries are discussedspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/EoceneOligoceneSequencesLower Tagus Basinjournal articleopen access