Geocronología de la sucesión arqueoestratigráfica de Los Estragales en la Terraza Compleja de Butarque (Valle del río Manzanares, Madrid)

In the low valley of Manzanares river, south of Madrid, is located the Butarque Complex Terrace formed by piling up of alluvial deposits of the Upper Pleistocene. In Perales del Río they have been excavated and picked up industries of the Middle Palaeolithic mainly in flint, in the sites of Los Estr...

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Detalles Bibliográficos
Autores: Pérez González, Alfredo José, Rubio Jara, Susana, Panera Gallego, Joaquín, Uribelarrea Del Val, David
Tipo de recurso: artículo
Fecha de publicación:2008
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:español
OAI Identifier:oai:docta.ucm.es:20.500.14352/52771
Acceso en línea:https://hdl.handle.net/20.500.14352/52771
Access Level:acceso abierto
Palabra clave:902(460.27)
Prehistoria
5504.05 Prehistoria
Descripción
Sumario:In the low valley of Manzanares river, south of Madrid, is located the Butarque Complex Terrace formed by piling up of alluvial deposits of the Upper Pleistocene. In Perales del Río they have been excavated and picked up industries of the Middle Palaeolithic mainly in flint, in the sites of Los Estragales 1, 2 and 3, dated by TL and OSL between the Eemien (5e) and MIS 4. The terraces overlapped with the Butarque Complex Terrace, at +11-12 m, +8m and La Gavia II, they have been deposited during the Heinrich events H4, H2 and H1, of agreement with the luminiscence datings.